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Detrital zircon U‐Pb geochronology and Hf isotope geochemistry of the Yukon‐
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Tanana terrane, Coast Mountains, southeast Alaska 5
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Mark E. Pecha1, George E. Gehrels1, William C. McClelland2, Nicky Giesler1, 9
Chelsi White1, Intan Yokelson1 10
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Department of Geosciences, University of Arizona, Tucson, AZ 85721 12
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Department of Geosciences, University of Iowa, Iowa City, IA 52242 15
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Submitted to Lithosphere, December 23, 2013 20
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Notetoreviewers:
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NumerousDRfilesaccompanythismanuscript,allofwhichareavailablefrom
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https://sites.google.com/a/laserchron.org/laserchron/home/seak‐ytt‐dr‐files
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*Contact author = Mark Pecha (mpecha@email.arizona.edu, 520-419-8934)
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ABSTRACT 32
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Pericratonal rocks in the western Coast Mountains, southeast Alaska, that have been 34
assigned to the Yukon‐Tanana terrane (YTT), include marine clastic strata with mafic to 35
felsic volcanic/plutonic rocks, and are subdivided into three distinct units: 1) Pre‐
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Devonian Tracy Arm Assemblage (TAA), 2) Devonian Endicott Arm Assemblage (EAA), 37
and 3) Mississippian‐Pennsylvanian Port Houghton Assemblage (PHA). U‐Pb 38
geochronologic and Hf isotopic analyses have been conducted on zircons separated 39
from 22 samples in order to evaluate provenance of the section. TAA samples are 40
dominated by Proterozoic (~0.9‐1.2, 1.6‐2.0 Ga) and Archean (2.5‐2.7 Ga) zircons. EAA 41
samples contain either prominent Silurian age peaks (438‐424 Ma) with juvenile HfT 42
values of +15 to +9, or are mainly composed of Devonian age peaks (403‐369 Ma) with 43
variable HfT values ranging from +13 to ‐8. PHA samples are dominated by Paleozoic 44
zircons with highly variable Hf values, and consist of either: 1) Silurian peaks (432‐425 45
Ma) with juvenile to intermediate Hf values of +15 to ‐1, or 2) late Devonian‐
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Mississippian age peaks (379‐351 Ma) with Hf mixing arrays displaying intermediate to 47
evolved sources (Hf values of +7 to ‐20). TAA samples strongly resemble previously 48
published detrital age spectra from the YTT and the northern miogeocline of western 49
North America. Several EAA and PHA samples contain Proterozoic age peaks similar to 50
those of the underlying TAA and the northern miogeocline, indicating a peri‐Laurentian 51
affinity for these assemblages as well. Possible connections between YTT in the Coast 52
Mountains and the Alexander terrane (AXT) may exist, as indicated by the presence of 53
juvenile Neoproterozoic (600‐545 Ma) and Early Paleozoic (530‐415 Ma) zircons in EAA 54
and PHA samples. Three options that account for the presence of Silurian‐Devonian 55
zircons and their associated Hf values are: 1) YTT and AXT are tectonically interleaved 56
at a scale previously not documented, 2) YTT and AXT both experienced ~360 and ~420 57
Ma arc magmatism, but formed along different plate boundaries, 3) YTT and AXT 58
evolved in the same 420‐360 Ma arc system, with YTT of western Laurentia origin and 59
AXT of non‐Laurentian origin. 4
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INTRODUCTION 62
The notion that most of the North American Cordillera is comprised of suspect terranes 63
was first introduced by Coney et al., 1980. Over the last 30+ years, geologists have 64
employed various geological, geophysical, and geochemical techniques in an attempt to 65
decipher the paleogeographic history of this collage of terranes (e.g., Gehrels and 66
Saleeby, 1987; Butler et al., 1989; Stevenson et al., 2000). Detrital zircon (DZ) analysis 67
has proven to be one of the most powerful tools at unraveling the complex histories of 68
these tectonically displaced crustal fragments (e.g., Gehrels et al. 1996; Beranek at al., 69
2010, 2012; Colpron and Nelson, 2011). Comprehensive DZ studies that include U‐Pb 70
ages in concert with Hf isotopic compositions provide insights into genetic relationships 71
between juxtaposed terranes, and also allow evaluation of their past interactions with 72
cratonal sources (Malone, 2012; Beranek et al., 2013; Tochilin et al., in press; Gehrels 73
and Pecha, in press). 74
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Previous U‐Pb geochronology of detrital zircons from the westernmost arm of Yukon‐
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Tanana terrane (YTT) in southeast Alaska is limited to a small number of analyses 77
conducted on a small number of samples. Recent technological advances (LA‐MC‐
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ICPMS, n=100, random grain selection) now allow for generation of a more robust 79
number of U‐Pb analyses per sample, and also acquisition of Hf isotopic compositions 80
from the same zircon crystals. 81
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GEOLOGIC BACKGROUND 83
The Yukon‐Tanana terrane is located within the Coast Mountains of southeast Alaska 84
and British Columbia, and underlies a large region of eastern Alaska, Yukon, and 85
northern British Columbia (Figure 1). Within eastern Alaska and Yukon Territory, YTT 86
has been described as a regionally metamorphosed pre‐Triassic assemblage that 87
includes Upper Paleozoic metasedimentary and metavolcanic rocks intruded by plutons 88
of various ages (Tempelman‐Kluit, 1976; Coney et al., 1980; Hansen, 1990; Mortensen, 5
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1991). Within the Coast Mountains of southeast Alaska, Berg et al. (1978) described a 90
similar belt of high‐grade quartzo‐feldspathic metasedimentary and silicic metavolcanic 91
rocks, referred to as the Tracy Arm terrane. Subsequent correlation of the Tracy Arm 92
terrane with the YTT to the north is primarily based on similar rock types and the 93
interpretation that these rocks formed in a continental margin setting (Gehrels et al., 94
1991, 1992; Saleeby and Rubin, 1989, 1990; McClelland et al. 1989, 1990; McClelland 95
1990; Samson et al. 1990a; Samson, 1990). 96
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The Coast Mountains assemblage of YTT is divided into three distinct units: 1) Pre‐
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Devonian Tracy Arm Assemblage (TAA), 2) Devonian Endicott Arm Assemblage (EAA), 99
and 3) Mississippian‐Pennsylvanian Port Houghton Assemblage (PHA) (Gehrels et al., 100
1991, 1992; McClelland et al., 1992). Figure 02 outlines the generalized stratigraphic 101
section of YTT in the Coast Mountains, including representative outcrop photographs of 102
each of the three main assemblages. Detailed geologic descriptions of these 103
assemblages can be found in Gehrels et al. (1991, 1992) and McClelland et al., (1992). 104
Location information and brief sample descriptions are available in DR Table 1. 105
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Tracy Arm Assemblage (TAA) 107
TAA is named for a series of shoreline exposures found within Tracy Arm (Figure 1) that 108
form the easternmost exposures of the YTT section within the Coast Mountains. The 109
rocks included in this unit were also incorporated into the original Tracy Arm terrane of 110
Berg et al., (1978) and Monger and Berg (1987). The dominant rock types are biotite 111
schist, gneiss, quartzite, and marble, with the majority being metamorphosed to at least 112
amphibolite facies. The metamorphic grade found in TAA is generally higher than within 113
EAA or PHA, likely due to its proximity to the mid‐Cretaceous to early Tertiary Coast 114
Plutonic Complex (Monger et al., 1982; Crawford et al. 1987; Brew et al., 1989; Stowell 115
and Hooper, 1990; Barker and Arth, 1990). These rocks are strongly deformed (Figure 2 116
(F)) and generally dip steeply (>80degrees) east‐northeast. TAA is interpreted to be a 117
pre‐Devonian continental margin assemblage that is correlated by (Gehrels et al., 1992; 6
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McClelland et al. 1991, 1992; Saleeby and Rubin, 1989, 1990) with the Yukon‐Tanana 119
terrane (Mortensen, 1991), Nisling terrane (Wheeler and McFeely, 1987), Dorsey 120
Complex (Roots et al., 2006), and Snowcap Complex (Colpron et al., 2006b) in the Yukon. 121
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Endicott Arm Assemblage (EAA) 123
The EAA represents a magmatic arc assemblage named for a series of shoreline 124
exposures along Endicott Arm (Figure 1). The sequence gradationally overlies the TAA 125
and predominantly consists of mafic to felsic metavolcanics, interbedded with volcanic‐
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rich metasediments (greywacke) and subordinate limestone (Gehrels et al., 1992). 127
Previous geochronologic analysis of EAA felsic metavolcanics yielded only Devonian ages 128
ranging from ~380‐360 Ma, leading to correlation with YTT in both the Yukon and 129
eastern Alaska (McClelland et al., 1991, 1992; Gehrels et al., 1991, 1992; Gehrels, 2001). 130
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Port Houghton Assemblage (PHA) 132
The PHA is characterized by quartz‐rich metaclastic rocks, including turbiditic facies, 133
interbedded with local mafic to felsic volcanic units and subordinate marble (Gehrels et 134
al., 1992). It also contains distinct metaconglomerate horizons with clasts consisting of 135
greywackes, quartzites, metarhyolites, and infrequent intermediate plutonic clasts. 136
Based on clast composition, these conglomerates are interpreted to have come from 137
the underlying EAA and TAA assemblages (Gehrels et al., 1992). 138
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ANALYTICAL METHODS 140
Approximately 15 kg of rock were collected for each detrital sample. Zircon grains were 141
extracted from the whole rock samples using traditional methods of jaw crushing and 142
pulverizing, followed by density separation using a Wifely table and heavy liquids 143
(diiodomethane: 3.32 g/cm3). The resulting heavy mineral fraction then underwent 144
separation using a Frantz LB‐1 magnetic barrier separator to isolate the zircons. A 145
representative split of the entire zircon yield of each sample was incorporated into a 1” 146
epoxy mount along with multiple fragments of the primary U‐Pb Sri Lanka (SL) zircon 7
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standard, and a few grains of each Hf standard (R33, Mud Tank, FC‐1, Plesovice, Temora, 148
91500, and Sri Lanka). The mounts were sanded down ~20 microns, polished using a 1‐
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micron polishing pad, and imaged by back‐scattered electrons (BSE) using a Hitachi S‐
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3400N scanning electron microscope (SEM). Prior to isotopic analysis, the mounts were 151
cleaned in an ultrasound bath of 1% HNO3 and 1% HCl in order to remove any residual 152
common Pb from the surface of the mounts. 153
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U‐Pb Geochronologic Analysis 155
U‐Pb geochronology of individual zircon crystals was conducted by laser ablation multi‐
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collector inductively coupled mass spectrometry (LA‐MC‐ICPMS) at the Arizona 157
LaserChron Center (Gehrels et al., 2006, 2008). The isotopic analyses involved ablation 158
of zircon using a Photon Machines Analyte G2 excimer laser (λ=193nm) coupled to a Nu 159
Instruments HR‐MC‐ICPS. Helium carried the ablated material into the plasma source of 160
the ICPMS, which is equipped with a flight tube of sufficient width such that U, Th, and 161
Pb isotopes are measured simultaneously. Depending on the size of the zircons, the 162
analyses were conducted with either a Faraday routine or an Ion Counter routine (see 163
DR Table 2 for specific methods used on each sample). 164
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The majority of the U‐Pb analyses were conducted with a 30 micron spot diameter using 166
a Faraday acquisition routine consisting of one 15 second integration on peaks with the 167
laser off (for backgrounds), 15 one‐second integrations with the laser firing, and a 30 168
second delay to ensure that the previous sample is completely purged from the ablation 169
chamber. Faraday detectors with 3x1011 ohm resistors measured 238U, 232Th, 208‐206Pb, 170
and discrete dynode ion counters measured 204Pb and 202Hg, all in static mode. Drill rate 171
was ~1 micron/second, resulting in a final ablation pit depth of ~15 microns. 172
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An Ion Counter routine was employed on samples that contained zircons that were too 174
small to accommodate a 30‐micron spot. These analyses consisted of one‐12 second 175
integration on peaks with the laser off (for backgrounds), 12 one‐second integrations 8
176
with the laser firing, and a 30 second delay to purge the previous sample. During this 177
routine, Faraday detectors measured 238U and 232Th, and discrete dynode ion counters 178
measured 208‐204Pb, also in static mode. Drill rate was ~1 micron/second, resulting in a 179
final ablation pit depth of ~12 microns. 180
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Approximately 105 analyses were completed on each detrital sample with one U‐Pb 182
measurement per grain. Grain selection was conducted randomly, with grains rejected 183
only on the basis of small size or the presence of cracks or inclusions. The use of high‐
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resolution BSE images for detrital samples and detailed CL images for igneous samples 185
provided assistance in grain selection and spot placement (See DR Table 1 for CL images 186
of representative zircons from each sample). 187
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Data reduction was accomplished using Nupmagecalc.xls, which is a standard Arizona 189
LaserChron Center reduction protocol. The specific filters used during the data 190
treatment are indicated in the notes at the end of the U‐Pb data table (DR Table 2). The 191
proximity of the YTT Coast Mountains assemblages to the Coast Plutonic Complex 192
(McClelland and Mattinson, 2000) has resulted in complex U‐Pb systematics including 193
the growth of metamorphic zircon, which is indicated by elevated U/Th values (>10) 194
(Harley et al., 2007; Hoskin and Schalteggar, 2003; Rubatto, 2002; Rubatto et al., 2001, 195
Williams, 2001). Additionally, a few younger analyses (DR Table 2 designated by blue 196
highlights) could not be discarded due to elevated U/Th values, but are not considered 197
to be robust as they are likely remnants of minute stringers that were not identified in 198
the field, yielding similar young ages to the metamorphic zircons. It is clear these young 199
Cenozoic grains are manifestations of local metamorphic perturbations and so they are 200
not considered further. 201
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Hf Isotopic Analysis 203
Hf isotope geochemistry of zircons was conducted by laser ablation multi‐collector 204
inductively coupled mass spectrometry (LA‐MC‐ICPMS) at the Arizona LaserChron 9
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Center following established analytical protocols reported in Cecil et al. (2011) and 206
Gehrels and Pecha (in press). 207
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An average of ~50 Hf analyses were conducted per detrital sample, with grains selected 209
to represent each main age peak, and to avoid crystals with discordant or imprecise 210
ages. CL images (examples for each sample are located in DR Table 1) were utilized for 211
navigation/spot location, ensuring all Hf analyses are within the same growth 212
zone/domain as the U‐Pb pit. All Hf laser pits were located directed on top of the earlier 213
U‐Pb analysis pit. Grains that could not accommodate the 40m Hf pit within the same 214
growth domain as the U‐Pb pit were excluded from Hf consideration. All Hf isotopic 215
data, including Hf‐evolution plots of individual samples are recorded in DR Table 3. 216
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Hf data are presented using Hf‐evolution diagrams (Figures 3), where initial 176Hf/177Hf 218
ratios are expressed in HfT notation, which represent the Hf isotopic composition at the 219
time of zircon crystallization relative to the chondritic uniform reservoir (CHUR) (Bouvier 220
et al., 2008). Internal precision for 176Hf/177Hf and Hf(0) is reported at the 1‐sigma level 221
in DR Table 3 and at the 2‐sigma level on the YTT epsilon Hf evolution plot (Figure 3). 222
Estimates of external precision are within 1‐2 epsilon units, given that nearly all session 223
averages of zircon standards are within this measure (DR Table 3). Following 224
established guidelines of Bahlburg et al. (2011) and Gehrels and Pecha (in press), HfT 225
values that are within 5 units of the depleted mantle (DM) (Vervoort and Blichert‐Toft, 226
1999) are referred to as juvenile in composition, values between and 5 and 12 units 227
below DM are considered intermediate, and values >12 units below DM are considered 228
evolved. Hf isotopic evolution of typical felsic crust is shown with arrows (Figures 3 and 229
4), and is based upon a 176Lu/177Hf ratio of 0.0115 (Vervoort and Patchett, 1996; Amelin 230
et al., 1999, 2000; Bahlburg et al., 2011). 231
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U‐Pb AGES and Hf ISOTOPIC RESULTS 10
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A total of 25 samples were collected from the Coast Mountains section of YTT with the 234
intent of obtaining both U‐Pb geochronologic and Hf isotopic data. All of the samples 235
yielded zircon; however, two samples (12MP17, 12MP18) collected within Carroll Inlet 236
and Bradfield Canal region produced low zircon yields. Final U‐Pb and Hf results for all 237
samples are reported in data repositories DR Table 2 and DR Table 3, respectively. To 238
assist with interpretation, samples are discussed below according to their stratigraphic 239
assignment (TAA, EAA, or PHA) within YTT. Due to significant spatial variations observed 240
within each assemblage, the samples are also evaluated on the general geographical 241
regions in which they occur (see Figure 1 for general outlines of the four regions (A‐D), 242
including sample locations). 243
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Tracy Arm Assemblage (TAA) 245
TAA in Bradfield Canal to Thomas Bay 246
TAA samples 12MP12 and 12MP13 consist of quartzite interbedded with marble and 247
biotite paragneiss. Sample 12MP12 is from the same location as 03GC0113 (Gehrels, 248
unpublished) and 12MP13 was collected from the same sequence as sample 90‐34 of 249
McClelland and Mattinson (2000). 12MP13 is dominated by an array of 250
Mesoproterozoic zircons (1000 – 1600 Ma) with HfT values clustering in the 251
intermediate range with more juvenile and evolved outliers. It also contains scattered 252
Paleoproterozoic grains (1800‐2000 Ma with HfT values ranging from +10 to ‐3) and 253
Archean zircons (2700‐2850 Ma) with juvenile to intermediate HfT values ranging from 254
+1 to ‐14. 255
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TAA in Tracy Arm to Port Snettisham 257
Sample 12MP33 is an orthoquartzite collected from the same locality in Tracy Arm as 258
sample 88GC414 of Gehrels et al. (1991). The U‐Pb age distribution is dominated by 259
Paleoproterozoic ages of 1736 to 2491 Ma (peaks at 1770 and 1828 Ma), with 260
subordinate Archean zircons ranging from 2521 to 2677 Ma (peak at 2668 Ma). The HfT 11
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ratios of the Paleoproterozoic zircons range from +4 to ‐13, and the Archean grains are 262
exclusively juvenile ranging from +7 to +2. 263
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An orthoquartzite (12MP41) collected in Port Snettisham produced similar 265
Paleoproterozoic ages ranging from 1737 to 2440 Ma (peaks at 1847, 1912, 2083Ma), 266
along with subordinate Archean ages ranging from 2543 to 2719 Ma (peak at 2713 Ma), 267
similar to 12MP33 collected in Tracy Arm. The Archean zircons are predominantly 268
juvenile (+7 to +2 HfT), while the Paleoproterozoic grains display evolved HfT values 269
clustering between +3 and ‐15. 270
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Overall, TAA samples are dominated by Paleoproterozoic grains ranging from ~1600–
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2100 Ma (age peaks of 1654, 1766, 1869, 2093 Ma), with subordinate groups from 273
~980–1386, 1420–1505, and 2420–2967 Ma (peaks of ~1104, 1179, 1459, 1503, 2557, 274
and 2720 Ma) (Figure 3). Hf results for TAA generally cluster in the intermediate range, 275
except for more negative HfT values for grains of 1800‐2000 Ma. 276
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Endicott Arm Assemblage (EAA) 278
EAA in Thorne Arm to Carroll Inlet 279
Aquartz‐eyerhyolite(12MP03)collectedinThorneArmandameta‐rhyolitein
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CarrollInlet(12MP08)yieldedweightedmeanagesof403.0±3.4Maand401.1±
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4.5Ma(2‐sigma),respectively.TheyalsodisplayrelativelyevolvedHfsources,
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with12MP03beingintermediatetoevolved(HfTvaluesclusteringfrom+5to‐3)
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and12MP08displayingmorenegativeepsilonHfvaluesof‐3to‐8HfT. 284
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EAA in Bradfield Canal to Thomas Bay 286
An EAA meta‐rhyolite (12MP19) collected in Blake Passage yielded a robust weighted 287
mean age of 377.3 ± 4.8 Ma (2‐sigma) and a tight cluster of juvenile epsilon Hf values of 288
+14 to +10, plotting just below the projected depleted mantle curve. Sample 12MP20, a 289
meta‐rhyolite collected in Thomas Bay, produced a weighted mean final age of 368.9 ± 12
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5.1 Ma (2‐sigma), and HfT values ranging from +11 to +2. Sample 12MP18, a meta‐
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conglomerate collected in Blake Passage only produced 3 zircons yielding limited data 292
and a 359 Ma peak. 293
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EAA in Port Houghton 295
12MP23 is a quartzite sample collected within Port Houghton, and is a duplicate of 296
sample 87GC81 reported in Gehrels et al. (1992). This sample yielded a prominent age 297
range of 390‐494 Ma (peak of 424 Ma), with subordinate age ranges of 504‐552,908‐
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1165, 1604‐1665, and 2425‐2710 Ma (peaks at 510, 1087, 1643, and 2678 Ma). The 299
epsilon Hf values for the main Silurian peak range from juvenile to intermediate (+13 to 300
+3), while the others predominantly range from intermediate to slightly evolved. 301
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EAA in Tracy Arm to Port Snettisham 303
Sample 12MP40 is an orthoquartzite from Snettisham Inlet that produced one main U‐
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Pb age peak at 380Ma displaying Juvenile to intermediate Hf values. 305
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EAA or Alexander terrane in Carroll Inlet 307
U‐Pb and Hf isotopic analyses were completed on a total of 11 samples collected within 308
the previously defined boundaries of the EAA section (Gehrels et al., 1992). Three of 309
these samples (12MP06, 12MP07, and 12MP09) were collected from a region within 310
Carroll Inlet that was previously assigned to the Alexander terrane (Saleeby 2000), 311
however, these rocks are completely surrounded by units that clearly belong to YTT. 312
The samples yielded U‐Pb ages of 438.5 ± 5.0, 423.6 ±4.8,and430.8±4.2Ma,and 313
juvenile Hf isotopic signatures, both of which are commensurate with known Alexander 314
terrane (AXT) samples from southeastern Alaska (Figures 4, and 5). Due to the high 315
degree of deformation and limited exposures of the contacts of these units, it is not 316
clear whether these samples are part of the Alexander terrane, or if they represent a 317
previously unrecognized signature of EAA. It is important to note that either of these 13
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options is possible. Therefore, these samples are grouped together and not included in 319
YTT composite distributions. 320
321
Port Houghton Assemblage (PHA) 322
PHA in Thorne Arm to Carroll Inlet 323
Samples 12MP04 (volcanic‐rich greywacke turbidite) and 12MP05 (pebble to cobble 324
conglomerate) were collected in Thorne Arm and yield unimodal age distributions of 325
379 and 372 Ma, respectively. Their HfT isotopic compositions range from juvenile to 326
intermediate (+14 to +3) for 12MP04 and (+11 to ‐4) for 12MP05, indicating a slightly 327
more evolved component. 328
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PHA in Bradfield Canal to Thomas Bay 330
Sample 12MP17 is the only PHA sample collected from this region. Unfortunately, the 331
sample only yielded 4 zircons resulting in three concordant U‐Pb ages (586, 1246, and 332
1661 Ma). Epsilon Hf values are coincident with other Proterozoic PHA zircons 333
displaying the same respective ages. 334
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PHA in Port Houghton 336
Two quartzite samples (12MP25 and 12MP24) collected within Port Houghton at the 337
type locality for PHA (Gehrels et al., 1991) yield very similar U‐Pb age distributions and 338
Hf isotopic signatures. These samples are dominated by Silurian zircons (432‐424 Ma) 339
with juvenile to intermediate (+15 to +2) Hf values. They also contain subordinate 340
juvenile to intermediate Cambrian (507‐510 Ma) and/or Neoproterozoic (~669 Ma) age 341
peaks. These samples also contain a dissemination of Proterozoic and Archean zircons 342
with variable Hf values (+10 to –16). 343
344
PHA in Tracy Arm to Port Snettisham 345
Samples 12MP39 and 12MP38 are conglomerates that yield similar analytical results. 346
Both samples are dominated by Late Devonian zircons (350 Ma age peaks), which 14
347
display evolved Hf values (+07 to –20) forming an elongated Hf mixing array. Whereas 348
both have a spread of Proterozoic zircons and isolated Archean zircons, sample 12MP39 349
has a prominent Paleoproterozic peak at ~1843 Ma and a robust Archean peak at 2968 350
Ma. 351
352
A total of seven PHA samples were collected and analyzed for both U‐Pb and Hf. A 353
composite probability distribution of all seven samples (Figures 3 and 4) illustrates that 354
PHA samples are dominated by 340 ‐390 Ma zircons (main peaks of 350 & 375 Ma), and 355
also include prominent age groups from 400‐470 Ma (peak of 431 Ma) and 550‐585 Ma 356
(peak of 569 Ma). The HfT values cluster systematically with age, and are 357
predominantly juvenile to intermediate, ranging from +15 to +5 (Figure 4). These 358
samples also have subordinate Mesoproterozoic age peaks of 1173, 1659, 1795, 1846, 359
and 1937 Ma, plus Archean peaks of 2605 and 2968 Ma. Epsilon Hf values from the Port 360
Houghton Arc system (~365 ‐345 Ma) are highly variable but systematic, displaying a 361
strong “pull‐down” from juvenile (HfT = +15 to +7 at ~365 Ma) to highly evolved (HfT = 362
‐12 to ‐20 by 345 Ma) Hf systematics (Figure 4, blue arrow top section). 363
364
COMPARISON OF U‐Pb and Hf DATA FROM YUKON‐TANANA TERRANE, ALEXANDER 365
TERRANE, AND UNITS OF UNCERTAIN TECTONIC AFFINITY 366
367
Crustal evolution of the YTT magmatic arc 368
The relatively large number of samples analyzed (N=22) combined with the temporal 369
variations observed in their Hf isotopic ratios allows for a robust evaluation of the YTT 370
arc evolution. Systematic changes in the source of parental magmas are revealed in the 371
near continuum of U‐Pb ages from the Early Silurian (~444 Ma) through Late Devonian 372
(~350 Ma), from both igneous and detrital samples. Two cycles of magma evolution, 373
one in the EAA and one in the PHA are evident within this section. Systematic 374
deviations or “pull‐downs” are observed in Hf isotopic ratios of both EAA and PHA 15
375
samples, and time‐series HfT plots were generated in order to illustrate their cyclical 376
maturation (Figure 4). 377
378
EAA magmatic arc system evolves progressively from a juvenile arc (Hf = +14 to +10) 379
beginning ~403 Ma to an evolved system (Hf = ‐5 to ‐7) by ~385 Ma (Figure 4). This 380
profound change signifies increasing interaction with continental crust and is 381
interpreted to reflect orogenesis during collision of the EAA arc system with Laurentian 382
basement. By ~380 Ma, the Hf isotopes abruptly swing back positive (Hf = +14 to +10) 383
to be juvenile in character, signifying a profound influx of material derived directly from 384
a depleted mantle source. This abrupt change is interpreted to be the manifestation of 385
a rapidly changing subduction system and correlates directly with the cessation of EAA 386
magmatism by ~369 Ma. 387
388
The PHA arc system follows a similar Hf evolution pattern to EAA, where it begins as a 389
juvenile (Hf = +13 to +10) system ~375 Ma and rapidly changes to a highly evolved (Hf 390
= ‐15 to ‐20) system by ~350 Ma. The trajectory of the PHA pull‐down is even steeper 391
and deeper than that of the EAA, signifying a second phase of continental crust 392
interaction with a greater percentage of crustal input into the melt. The intervening 393
time between the EAA and PHA systems is manifested in the change from negative Hf 394
values to positive Hf values, representing the recognized unconformity between the 395
two assemblages. 396
397
Evaluation and proposed reassignment of three EAA samples to the AXT 398
Three samples (12MP06, 12MP07, and 12MP09) collected within the Endicott Arm 399
Assemblage resulted in U‐Pb ages of 438.5 ± 5.0, 423.6 ±4.8,and 430.8±4.2 Ma(2‐
400
sigma weighted averages),respectively, with juvenile Hf isotopic signatures (Hf = +15 401
to +10), which are both commensurate with known Alexander terrane samples from the 402
Coast Mountains section (Figure 4). Kolmogorov‐Smirnoff (K‐S) statistical comparisons 403
of these samples with published AXT samples (Gehrels, 1996; Tochilin et al., in press) 16
404
yield P values > 0.05, indicating they are not statistically different in their U‐Pb age 405
distributions (DR‐4 contains all the K‐S comparisons). The two most likely scenarios that 406
account for the presence of these Silurian zircons within the EAA section are: 1) the 407
units represent a displaced section of AXT that is tectonically interleaved within the EAA 408
section, or 2) the rocks are actually part of the EAA section, therefore indicating a much 409
earlier juvenile magmatic history than previously recognized in any YTT samples. Due to 410
the high degree of deformation and limited exposures of the contacts of these units, it is 411
not clear geologically whether these samples are actually part of the AXT or if they 412
represent a previously unrecognized signature of EAA. However, in support of earlier 413
correlations of these units with AXT (Saleeby, 2000), we now favor the interpretation 414
that these units are actually part of the AXT stratigraphy, structurally intercalated within 415
the EAA section. For future comparison purposes, these samples are shown separately 416
from other EAA samples in the probability density distributions and not included within 417
EAA distributions. They are grouped together to represent AXT and provide strikingly 418
similar isotopic signatures to published AXT samples (Figures 4 and 5). 419
420
U‐Pb and Hf comparisons with the Alexander terrane 421
The Alexander terrane within southeastern Alaska has been described as a primitive 422
island arc system consisting of Neoproterozoic‐Silurian volcanic, plutonic, volcaniclastic 423
units, along with Devonian‐Triassic volcanics and volcaniclastics with subordinate 424
conglomerate and limestone (Gehrels and Saleeby, 1987; Gehrels et al., 1996; Gehrels 425
and Boghossian, 2000). Nd‐Sr signatures for AXT are juvenile (Samson and Patchett, 426
1991), as is the Hf signature for AXT in the Coast Mountains (Cecil et al., 2011; Tochilin 427
et al., in press; White et al., in preparation). The enduring consistency of age and 428
isotopic character of the AXT allows for stringent evaluation with respect to the now 429
adjacent YTT (Figure4 & 5). 430
431
All YTT samples are statistically distinguishable (P values < 0.05) from all AXT samples in 432
U‐Pb age and Hf isotopes, as was expected based on their different geologic histories 17
433
and inferred environments of formation. As described earlier, three samples (two meta‐
434
trondjemite and one metarhyolite) collected within the EAA section (12MP06, 12MP07, 435
and 12MP09) have U‐Pb and Hf signatures identical to known AXT samples in the Coast 436
Mountains (Tochilin et al., in press). Therefore, these samples likely are pieces of AXT 437
that has been tectonically interleaved within the EAA. If this is the case, then detrital 438
signatures found within PHA detrital samples provide possible links of AXT and YTT 439
(Coast Mountains) by Mississippian time (~350 Ma) and possibly earlier. Figure 4 shows 440
that many EAA and PHA detrital samples have remarkably similar U‐Pb peak age peaks 441
(~425, 480, and 570 Ma), in addition to similar Hf isotopic characteristics (predominantly 442
juvenile +15 to +10) of the adjacent AXT. Two PHA quartzite samples (12MP24 and 443
12MP25) that were collected at the type locality of PHA within Port Houghton also have 444
prominent juvenile Silurian (432 and 425 Ma, respectively) zircons that are coincident 445
with published AXT distributions. They also contain older AXT signatures (~580‐550 Ma, 446
juvenile) and (~490‐460 Ma, juvenile to intermediate) as illustrated in the pink fields in 447
Figure 4. Additional PHA and even a few EAA samples also contain zircons with similar 448
Hf isotopic character. 449
450
Three possible scenarios that account for the presence of similar Neoproterozoic‐Early 451
Paleozoic age populations and Hf isotopic signatures are: 1) YTT and AXT are tectonically 452
interleaved at a scale previously not documented, as suggested by the data from the 453
EAA section, 2) YTT and AXT both experienced ~420 to ~350 Ma arc magmatism, but 454
formed along different plate boundaries, 3) YTT and AXT evolved in the same ~420‐350 455
Ma arc system, with YTT of western Laurentia origin and AXT with presumed ties to the 456
Baltica margin. (i.e. Soja, 1994, 2008; Bazard et al., 1995; Soja and Krutikov, 2008; Grove 457
et al., 2008; Bodgett, 2010; Miller et al., 2010, 2011; Colpron and Nelson, 2009, 2011). 458
459
Additional comparison with Banks Island Assemblage (BIA) and Saint Elias Mountains 460
Based on the profusion of highly folded metaclastic quartzite and marble sections within 461
BIA and YTT, it has been suggested that BIA is a displaced fragment of YTT (Gehrels and 18
462
Boghossian, 2000; Boghossian and Gehrels, 2000). In order to evaluate this idea, U‐Pb 463
ages and Hf isotopes were overlaid with Tochilin et al., in review (Figure 5). Both the U‐
464
Pb and Hf results indicate low similarity between the datasets. 465
466
U‐Pb geochronologic and Hf isotopic data are available from the BIA preserved in the 467
Coast Mountains, west of YTT and AXT (Tochilin et al., in press). These data provide 468
critical insights as they yield similar ages and Hf evolutions of Silurian and early 469
Devonian aged zircons, but also have profoundly different Proterozoic age peak (i.e. 470
900‐600 Ma grains). Many BIA samples show a wide range of display large deflections 471
into highly evolved epsilon Hf space, similar to Devonian EAA arc evolution. Based on 472
these comparisons, it is clear that YTT and AXT are distinct from one another. 473
474
Based on inferences in the published literature (e.g. Soja, 1994, 2008; Bazard et al., 475
1995; Soja and Krutikov, 2008; Grove et al., 2008; Bodgett, 2010; Miller et al., 2010, 476
2011; Colpron and Nelson, 2009, 2011) regarding the connection between AXT and the 477
Baltic region, a DZ comparison plot of YTT and the greater Circum‐Arctic region was 478
generated (DR‐4). This figure illustrates mainly Laurentian matches (i.e., NE Canadian 479
Shield for Archean (~2900‐2500 Ma) and Paleoproterozoic (~2000‐1600 Ma)). It also 480
illustrates the possible connection between EAA and PHA samples to the AXT 481
Neoproterozoic (580‐550 Ma) and Early Paleozoic (485‐415 Ma) zircons, but nothing else 482
is apparent regarding any connection with circum‐Baltic regions. 483
484
Comparison with existing YTT DZ U‐Pb data 485
Detrital zircon U‐Pb age comparisons were made with previously published YTT detrital 486
zircon analyses from SE Alaska (Gehrels et al 1991, 1992; Gehrels 2001, 2002) and from 487
Yukon and eastern Alaska (Nelson and Gehrels, 2007; Dusel‐Bacon et al., 2003; Dusel‐
488
Bacon et al., 2013; Colpron et al, 2006) (Figure 5). The newly acquired U‐Pb data are 489
nearly identical to the published data from YTT in southeast Alaska, and are dominated 490
by Devonian‐Mississippian arc derived zircons, with significant Paleoproterozic (main 19
491
peaks ranging from ~1700 to ~2000 Ma) input and subordinate Archean peaks (Fig. 5). 492
DZ age comparisons with spectra from inboard sections of YTT (Nelson and Gehrels, 493
2007; Dusel‐Bacon et al., 2003; Dusel‐Bacon et al., 2013; Colpron et al, 2006) also yield 494
similar U‐Pb results (Figure 5). It is noted that the main Paleoproterozoic age peaks 495
from the inboard YTT samples are ~5‐10% older (main peaks ~1950 Ma) than those 496
observed in the Coast Mountains section (main peaks ~1840 Ma). 497
498
Unfortunately, Hf data do not exist for the YTT in eastern Alaska and Yukon, precluding 499
additional comparisons. 500
501
Comparison between YTT and North American passive margin strata 502
Linking the YTT Coast Mountains assemblage to a cratonal source is the first‐order test 503
of establishing YTT provenance. The passive margin strata (miogeocline) of North 504
America (NA) offer the most comprehensive NA cratonal signature because it samples 505
detritus from the entirety of the watershed, instead of select regions or provinces. 506
Gehrels et al. (1995) and Gehrels and Pecha (in press) provide six proxies for the North 507
American DZ U‐Pb and Hf isotopic signatures at various latitudes from Alaska, USA to 508
Sonora, Mexico. Kolmogorov‐Smirnoff (K‐S) statistical comparisons with individual 509
samples from all six of the reference miogeoclinal transects reveals multiple similarities 510
between our TAA data and the northern British Columbia (NBC), southern British 511
Columbia (SBC), and Nevada (Nev), and Sonora (SON) transects (refer to DR Table 4 for 512
the K‐S test results). The abundance of P‐values >0.05 when comparing individual 513
samples between YTT and miogeoclinal transects provides support for Laurentian 514
affinity of YTT Coast Mountains, particularly the pre‐Devonian Tracy Arm Assemblage. 515
516
Normalized and stacked U‐Pb probability density plots (Figure 5) display important 517
visual comparisons between a composite YTT U‐Pb spectrum and northern Cordilleran 518
transects of the miogeocline (AK, NBC, and SBC), suggesting a Laurentian affinity for the 519
YTT. This is illustrated with the abundance of similar Mesoproterozoic (1.0‐1.2 and ~1.4 20
520
Ga), Paleoproterozoic 1.6‐2.0 Ga, and Archean (2.5‐3.0 Ga) aged zircons. The most 521
convincing similarities exist with Liard (NBC), Kindle (NBC), Adams (AK), Nation River 522
(AK), Spray (SBC), Sassenach (SBC), and Whitehorse (SBC), Chinle (Nev), Osgood (Nev), 523
and Geertsen (Nev) samples from the miogeocline (see DR Table 4 for additional 524
comparison PDP plots and K‐S statistics from individual samples). 525
526
In addition to the U‐Pb data, epsilon Hf comparisons (Figure 6) with all miogeoclinal 527
transects were conducted. The Hf results also indicate a probable Laurentian origin for 528
YTT Coast Mountains. Similar Hf isotopic evolution in Mesoproterozoic (1.0‐1.2 and ~1.4 529
Ga), Paleoproterozoic 1.6‐2.0 Ga, and Archean (2.5‐3.0 Ga) grains as zircons in the 530
northern Cordilleran transects provides an additional line of evidence for a Laurentian 531
origin of those zircons. With the exception of the California‐Sonora miogeoclinal 532
transects, all other North American transects contain grains that generally fill the 533
representative YTT interpreted fields in epsilon Hf space. 534
535
CONCLUSIONS 536
U‐Pb geochronology and Hf isotope geochemistry of the YTT in the Coast Mountains, 537
southeastern Alaska provides important insights into the evolution and paleogeography 538
of YTT and its neighboring terranes. Our new data support earlier correlations of the 539
YTT in the Coast Mountains with the YTT in eastern Alaska and the Yukon (Gehrels et al., 540
1991, 1992; Saleeby and Rubin, 1989, 1990; McClelland et al. 1989, 1990; McClelland 541
1990; Samson et al. 1990a; Samson, 1990). We have also demonstrated that the YTT is 542
likely peri‐Laurentian in affinity, through comparisons of our detrital zircon U‐Pb age 543
spectra and Hf isotopic compositions with reference datasets from passive margin strata 544
of North America. This is most evident for the pre‐Devonian TAA, which exhibits U‐Pb 545
age spectra that are statistically indistinct from many miogeoclinal samples from British 546
Columbia (Gehrels et al., 1995; Gehrels and Pecha, in press) (DR‐Table 4). 547
21
548
Two cycles of magma evolution, one in the Devonian EAA and one in the Mississippian 549
PHA are evident within this section. The EAA magmatic arc system evolves progressively 550
from a juvenile arc (Hf = +14 to +10) beginning ~403 Ma to an evolved system (Hf = ‐5 551
to ‐7) by ~385 Ma (Figure 4). This change in Hf isotopic data signifies increasing 552
interaction with continental crust and is interpreted to reflect orogenesis during 553
collision of the EAA arc system with Laurentian basement. The PHA arc system follows a 554
similar Hf evolution pattern to EAA, where it begins as a juvenile (Hf = +13 to +10) 555
system ~375 Ma and rapidly changes to a highly evolved (Hf = ‐15 to ‐20) system by 556
~350 Ma. The trajectory of the PHA Hf pull‐down is steeper than that of the EAA, 557
signifying a second phase of continental crust interaction with a greater percentage of 558
crustal input into the melt. The intervening time between the EAA and PHA systems is 559
manifested in the change from negative Hf values to positive Hf values, representing 560
the recognized unconformity between the two assemblages. 561
562
The presence of juvenile Neoproterozoic (600‐550 Ma) and Early Paleozoic (505‐419 563
Ma) zircons in multiple Port Houghton Assemblage detrital samples yields important 564
paleogeographic implications for the interaction of YTT in the Coast Mountains and the 565
AXT (Figure 4). These data suggest, that AXT was close enough to the peri‐Laurentian 566
YTT to contribute detritus into the PHA basin by Late Devonian to Early Mississippian 567
time. While we cannot be certain that these grains came exclusively from the AXT, this 568
neighboring juvenile terrane is the most likely scenario for being the source of these 569
zircons with such distinct U‐Pb and Hf signatures. 570
571
Three samples collected within the EAA section (12MP06, 12MP07, and 12MP09) 572
resulted in U‐Pb ages (2‐sigma weighted averages of 438.5 ± 5.0, 423.6 ±4.8,and430.8
573
±4.2Ma,respectively) and juvenile Hf isotopic signatures, both of which are 574
commensurate with known Alexander terrane samples from the Coast Mountains 575
section (Figures 4 and 5). These results yield three possible scenarios to explain the 576
potential genetic relationship between YTT (Coast Mountains section only) and AXT: 1) 22
577
YTT and AXT are tectonically interleaved at a scale previously not documented, 2) YTT 578
and AXT both experienced ~360 and ~420 Ma arc magmatism, but formed along 579
different plate boundaries, 3) YTT and AXT evolved in the same 420‐360 Ma arc system, 580
with YTT of western Laurentia origin and AXT of non‐Laurentian affinity. 581
582
ACKOWLEDGEMENTS 583
WerecognizetheNationalScienceFoundationforitssupportofthisproject(NSF
584
EAR#0947904)andforitscontinuedsupportoftheArizonaLaserChronCenter
585
(NSFEAR#1032156).WethankClaytonLoehn,KennethKanipe,GaylandSimpson,
586
BethWelke,RyanGraham,andCooperKowalskifortheirtechnicalsupportin
587
helpingpreparethezirconseparatesandacquiringtheSEMimages.Wealsothank
588
PeterGDeCelles,BrianMahoneyandNedBrownfortheircriticalinsights,which
589
greatlyimprovedthequalityofthismanuscript.Finally,weacknowledgeCaptain
590
DonWillsonforsharinghisnauticalexpertiseandlogisticalsupportwhile
591
navigatingthewatersofsoutheastAlaska.
592
593
REFERENCES 594
Amelin, Y., Lee, D.C., Halliday, A.N., Pidgeon, R.T., 1999, Nature of the Earth’s earliest 595
crust from Hf isotopes in single detrital grains: Nature, v. 399, p. 252‐255. 596
Amelin, Y., Lee, D.‐C., Halliday, A.N., 2000, Early‐middle Archean crustal evolution 597
deduced from Lu‐Hf and U‐Pb isotopic studies of single zircon grains: Geochemica et 598
Cosmochimica Acta, v. 64, no. 24, p. 4205‐4225. 599
Bahlburg, H., Vervoort, J.D., DuFrane, S.A., Carlotto, V., Reimann, C., and Cardenas, J., 600
2011, The U‐Pb and Hf isotope evidence of detrital zircons of the Ordovician 601
Ollantaytambo Formation, southern Peru, and the Ordovician provenance and 602
paleogeography of southern Peru and northern Bolivia: Journal of South American Earth 603
Sciences, v. 32, p. 196‐209. 604
Barker, f., and Arth, J.G., 1990, Two traverses across the Coast batholith, southeastern 23
605
Alaska. In The nature and origin of Cordilleran magmatism. Edited by J.L. Anderson, 606
Geological Society of America, Memoir 174, p. 395‐405. 607
Bazard, D.R., Butler, R.F., Gehrels, G.E., Soja, C.M., 1995, Early Devonian paleomagnetic 608
data from the Lower Devonian Karheen Formation suggest Laurentia‐Baltica connection 609
for the Alexander terrane: Geology, v. 23, p. 707‐710. Doi: 10.1130/0091‐
610
7613(1995)023<0707:EDPDFT>2.3.CO;2. 611
Beranek, L.P., Mortensen, J.K., Lane, L.S., Allen, T.L., Fraser, T.A., Hadlari, T., Zantvoort, 612
W.G., 2010, Detrital zircon geochronology of the western Ellesmerian clastic wedge, 613
northwestern Canada: Insights on Arctic tectonics and the evolution of the northern 614
Cordilleran miogeocline: Geological Society of America Bulletin, v. 122 (11‐12), p. 1899‐
615
1911. 616
Beranek, L.P., van Staal, C.R., Gordee, S.M., McClelland, W.C., Israel, S., Mihalynuk, M.G., 617
2012, Tectonic significance of Upper Cambrian‐Middle Ordovician mafic volcanic rocks 618
on the Alexander terrane, Saint Elias Mountains, northwestern Canada: The Journal of 619
Geology, v. 120, p. 293‐314, doi: 10.1086/664788. 620
Beranek, L.P., van Staal, C.R., McClelland, W.C., Israel, S., Mihalynuk, M.G., 2013, Detrital 621
zircon Hf isotopic compositions indicate a northern Caledonian connection for the 622
Alexander terrane: Lithosphere, v. 5, no. 2, p. 163‐168. 623
Berg, H.C., Jones, D.L., Coney, P.J., 1978, Map showing pre‐Cenozoic 624
tectonostratigraphic terranes of southeastern Alaska and adjacent areas: United States 625
Geological Surveys, Open‐file Report 78‐1085. 626
Blodgett, R., 2010, Upper Ordovician‐Middle Devonian paleobiogeographic signals from 627
shelly faunas of the Alexander terrane, southeast Alaska: Geological Society of America, 628
Abstracts with Programs, v. 42 (5), p. 573. 629
Boghossian, N.D., and Gehrels, G.E., 2000, Nd isotopic signature of metasedimentary 630
pendants in the Coast Mountains between Prince Rupert and Bella Coola, British 24
631
Columbia, in: Stowell, H.H., McClelland, W.D. (Eds.). Tectonics of the Coast Mountains, 632
Southeastern Alaska and British Columbia: Geological Society of America Special Paper 633
343, p. 77‐78. 634
Bouvier, A., Vervoort, J.D., and Patchett, J.D., 2008, The Lu‐Hf and Sm‐Nd isotopic 635
composition of CHUR: Constraints from unequilibrated chondrites and implications for 636
the bulk composition of terrestrial planets: Earth and Planetary Science Letters, v. 273, 637
p. 48‐57. 638
Brew, D.A., Ford, A.B., Himmelberg, G.R., 1989, Evolution of the western part of the 639
Coast plutonic‐metamorphic complex, southeastern Alaska, USA: a summary. In 640
Evolution of metamorphic belts. Edited by J.S. Daly, R.A. Cliff, B.W.D. Yardley, Geological 641
Society of London, Special Publication 43, p. 447‐452. 642
Butler, R.F., Gehrels, G.E., McClelland, W.C., May, S.R., 1989, Discordant paleomagnetic 643
poles from the Canadian Coast Plutonic Complex: Regional tilt rather than large‐scale 644
displacement?: Geology, v. 17, no. 8, p. 691‐694, doi: 10.1130/0091‐7613(1989). 645
Cecil, R., Gehrels, G., Patchett, J., Ducea, M., 2011, U‐Pb‐Hf characterization of the 646
central Coast Mountains batholith: Implications for petrogenesis and crustal 647
architecture: Lithosphere, v. 3 (4), p. 247‐260. 648
Colpron, M., and Nelson, J., 2009, A Paleozoic Northwest Passage: incursion of 649
Caledonian, Baltican and Siberian terranes into eastern Panthalassa, and the early 650
evolution of the North American Cordillera, in Cawood, P.A. and Kroner, A., eds., Earth 651
Accretionary Systems in Space and Time: The Geological Society, London, Special 652
Publications, v. 318, p. 273–307. 653
Colpron, M., and Nelson, J., 2011, A Paleozoic NW passage and the Timanian Caledonian 654
and Uralian connections of some exotic terranes in the North American Cordillera, in 655
Spencer, A.M., Embry, A.F., Gautier, D.L., Stoupakova, A.V., and Sorensen, K., eds., Arctic 656
Petroleum Geology. Geological Society, London, memoirs, v. 35, p. 463‐484. 25
657
Coney, P.J., Jones, D.L., Monger, J.W.H., 1980, Cordilleran suspect terranes: Nature 658
(London), v. 288, p. 329‐333. 659
Crawford, M.L., Hollister, L.S., Woodsworth, G.J., 1987, Crustal deformation and regional 660
metamorphism across a terrane boundary, Coast plutonic complex, British Columbia: 661
tectonics, v. 6, p. 343‐361. 662
Dickinson, W.R., and Gehrels, G.E., 2009, Use of U‐Pb ages of detrital zircons to infer 663
maximum depositional ages of strata: A test against a Colorado Plateau Mesozoic 664
database: Earth and Planetary Science Letters, v. 288, p. 115‐125. 665
Dusel‐Bacon, C., Wooden, J.L., Hopkins, M.J., 2003, U‐Pb zircon and geochemical 666
evidence for bimodal mid‐Paleozoic magmatism and syngenetic base‐metal 667
mineralization in the Yukon‐Tanana terrane, Alaska: Geological Society of America 668
Bulletin, v. 116, no. 7‐8, p. 989‐1015. Doi 10.1130/B25342.1. 669
Dusel‐Bacon, C., Day, W.C., Aleinikoff, J.N., 2013, Geochemistry, petrography, and zircon 670
U‐Pb geochronology of Paleozoic metaigneous rocks in the Mount Veta are of east‐
671
central Alaska: Implications for the evolution of the westernmost part of the Yukon‐
672
Tanana terrane: Canadian Journal of Earth Sciences, v. 50, no. 8, p. 826‐846. Doi: 673
10.1139/cjes. 674
Gehrels, G.E., 2000a, Geology and U‐Pb geochronology of the western flank of the Coast 675
Mountains between Juneau and Skagway, southeast Alaska, In Tectonics of the Coast 676
Mountains, southeast Alaska and coastal British Columbia. Edited by H.H. Stowell and 677
W.C. McClelland, Geological Society of America, Special Paper 343, p. 213‐233. 678
Gehrels, G.E., 2002, Detrital zircon geochronology of the Taku terrane, southeast Alaska: 679
Canadian Journal of Earth Sciences, 39, p. 921‐931. 680
Gehrels G.E., and Saleeby, J.B., 1987, Geological framework, tectonic evolution, and 681
displacement of the Alexander terrane: tectonics, v. 6, no.2, p. 151‐173. 682
Gehrels, G.E., and Ross, G.M., 1998, Detrital zircon geochronology of Neoproterozoic to 26
683
Permian miogeoclinal strata in British Columbia and Alberta: Canadian Journal of Earth 684
Sciences, v. 35, p. 1380‐1401. 685
Gehrels, G.E., and Kapp, P.A., 1998, Detrital zircon geochronology and regional 686
correlation of metasedimentary rocks in the Coast Mountains, southeastern Alaska: 687
Canadian Journal of Earth Sciences, v. 35, p. 269‐279. 688
Gehrels, G.E., and Boghossian, N.D., 2000, Reconnaissance geology and U‐Pb 689
geochronology of the west flank of the Coast Mountains between Bella Coola and Prince 690
Rupert, coastal British Columbia, in: Stowell, H.H., McClelland, W.C., Eds., tectonics of 691
the Coast Mountains, Southeastern Alaska and British Columbia. Geological Society of 692
America Special Paper 343, p. 61‐76. 693
Gehrels, G.E., and Pecha, M.E., in press, Detrital zircon U‐Pb geochronology and Hf 694
isotope geochemistry of Paleozoic and Triassic passive margin strata of western North 695
America, Geosphere, 696
Gehrels, G.E., McClelland, W.C., Samson, S.D., Patchett, P.J., Brew, D.A., 1991, U‐Pb 697
geochronology of Late Cretaceous and early Tertiary plutons in the northern Coast 698
Mountains batholith: Canadian Journal of Earth Sciences, v. 28, p. 899‐911. 699
Gehrels, G.E., McClelland, W.C., Samson, S.D., Patchett, P.J., Orchard, M.J., 1992, 700
Geology of the western flank of the Coast Mountains between Cape Fanshaw and Taku 701
Inlet, southeastern Alaska: Tectonics, v. 11, no. 3, p. 567‐585. 702
Gehrels, G.E., Dickinson, W.R., Ross, G.M., Stewart, J.H., and Howell, D.G., 1995, Detrital 703
zircon reference for Cambrian to Triassic miogeoclinal strata of western North America: 704
Geology, v. 23, p. 831‐834. 705
Gehrels, G.E., Butler, R.F., and Bazard, D.R., 1996, Detrital zircon geochronology of the 706
Alexander terrane, southeastern Alaska: Geological Society of America Bulletin, v. 108, 707
p. 722‐734. 708
Gehrels G.E., Valencia, V., Pullen, A., 2006, Detrital zircon geochronology by Laser‐
27
709
Ablation Multicollector ICPMS at the Arizona LaserChron Center, in Loszewski, T., and 710
Huff, W., eds., Geochronology: Emerging opportunities, Paleontology Society Short 711
Course: paleontology Society Papers, v. 11, 10 p. 712
Gehrels, G.E., Valencia, V., Ruiz, J., 2008, Enhanced precision, accuracy, efficiency, and 713
spatial resolution of U‐Pb ages by laser ablation‐multicollector‐inductively coupled 714
plasma‐mass spectrometry: Geochemistry, Geophysics, Geosystems, v. 9, Q03017, 715
doi:10.1029/2007GC001805. 716
Gehrels, G.E., Rusmore, M., Woodsworth, G., Crawford, M., Andronicos, C., Hollister, L., 717
Patchett, J., Ducea, M., Butler, R., Klepis, K., Davidson, C., Friedman, R., Haggart, J., 718
Mahoney, B., Crawford, W., Pearson, D., and Girardi, J., 2009, U‐Th‐Pb geochronology of 719
the Coast Mountains batholith in north‐coastal British Columbia: Constraints on age and 720
tectonic evolution: Geological Society of America Bulletin, v. 121, p. 1341‐1361. 721
Grove, M., Gehrels, G., Cotkin, S., Wright, J., Zou, H., 2008, Non‐Laurentian cratonal 722
provenance of Late Ordovician eastern Klamath blueschists and a link to the Alexander 723
terrane, in Wright, J., and Shervais, J., eds., Ophiolites, arcs, and batholiths: A tribute to 724
Cliff Hopson: Geological Society of America Special Paper 438. P. 223‐250. 725
Hadlari, T., Davis, W.J., Dewing, K., Heaman, L.M., Lemieux, Y., Ootes, L., Pratt, B.R., Pyle, 726
L.J., 2012, Two detrital zircon signatures for the Cambrian passive margin of northern 727
Laurentia highlighted by new U‐Pb results from northern Canada: Geological Society of 728
America Bulletin, v. 124 (7‐8), p. 1155‐1168. 729
Hansen, V.L., 1990, Yukon‐Tanana terrane: A partial acquittal: Geology, v. 18, p. 365‐
730
369. 731
Harley, S., Kelly, N., Moller, A., 2007, Zircon behavior and the thermal histories of 732
mountain chains: Elements, v. 3, p. 25‐30. 733
Hoffman, P.F., 1989, Precambrian geology and tectonic history of North America, in 734
Bally, A.W., and Palmer, A.R., eds., The geology of North America ‐ An overview: 28
735
Boulder, CO, Geological Society of America, Geology of North America, v. A, p, 447‐512. 736
Hoskin, P., and Schaltegger, U., 2003, The composition of zircon and igneous and 737
metamorphic petrogenesis in zircon: Rev. Mineral. Geochem., v. 53, edited by J. 738
Hanchar and P. Hoskin, Mineral. Soc. Of Am., Washington, D.C., p. 27‐62. 739
Lemieux, Y., Hadlari, T., and Simonetti, A., 2011, Detrital zircon geochronology and 740
provenance of Devono‐Mississippian strata in the northern Canadian Cordilleran 741
miogeocline: Canadian Earth Sciences, v. 48, p. 515‐541. 742
Ludwig, K.R., 2008, Isoplot 3.60. Berkeley Geochronology Center, Special Publication No. 743
4, 77 p. 744
Malone, S.J., 2012, Tectonic evolution of northern Ellesmere Island: Insights from the 745
Pearya terrane, Ellesmerian clastic wedge and Sverdrup Basin: PhD diss., University of 746
Iowa. 747
McClelland, W.C., and Mattinson, J.M., 2000, Cretaceous‐Tertiary evolution of the 748
western Coast Mountains, central southeastern Alaska, in: Stowell, H.H., McClelland, 749
W.C., Eds., tectonics of the Coast Mountains, Southeastern Alaska and British Columbia. 750
Geological Society of America Special Paper 343, p.159‐182. 751
McClelland, W.C., Gehrels, G.E., Samson, S.D., and Patchett, P.J., 1991, Protolith 752
relations of the Gravina belt and Yukon‐Tanana terrane in central southeastern Alaska: 753
Journal of Geology, v. 100, p. 107‐123. 754
McClelland, W.C., Gehrels, G.E., Samson, S.D., and Patchett, P.J., 1992, Structural and 755
geochronologic relations along the western flank of the Coast Mountains batholith: 756
Stikine River to Cape Fanshaw, central southeastern Alaska: Journal of Structural 757
Geology, v. 14, p. 475‐489. 758
Miller, E.L., Gehrels, G.E., Pease, V., Sokolov, S., 2010, Paleozoic and Mesozoic 759
stratigraphy and U‐Pb detrital zircon geochronology of Wrangell Island, Russia: 760
Constraints on Paleogeography and paleocontinental reconstructions of the Arctic: 29
761
American Association of Petroleum Geologists Bulletin, v. 94, p. 665‐692. 762
Miller, E.L., Kuznetsov, N., Soboleva, A., Udoratina, O., Grove, M.J., Gehrels, G.E., 2011, 763
Baltica in the Cordillera?” Geology, v.39, p. 791‐794. 764
Monger, J.W.H., and Berg, H.C., 1987, Lithotectonic terrane map of western Canada and 765
southeastern Alaska: United States Geological Survey, Miscellaneous Field Studies Map, 766
MF‐1874‐B. 767
Mortensen, J.K., 1992, Pre‐mid‐Mesozoic tectonic evolution of the Yukon‐Tanana 768
terrane, Yukon and Alaska: Tectonics, v. 11, no. 4, p. 836‐853, doi:10.1029/91TC01169. 769
Nelson, J.A., and Gehrels, G., 2007, Detrital zircon geochronology and provenance of the 770
southeastern Yukon‐Tanana terrane, Canadian Journal of Earth Sciences, v. 44, p. 297‐
771
316 doi: 10.1139/E06‐105. 772
Roots, C.F., Nelson, J.L., Simard, R.L., Mihalynuk, M., Harms, T.A., Friedman, R., and 773
Heaman, L., 2006, Continental fragments, Paleozoic arcs, and overlapping Triassic 774
sediments in the pericratonic belt, northern British Columbia and southern Yukon, In 775
Paleozoic evolution and metallogeny of pericratonic terranes at the ancient Pacific 776
margin of North America, Canadian and Alaskan Cordillera, edited by M. Colpron and J.L. 777
Nelson: Geological Association of Canada, Special Paper 45, p. 153‐177. 778
Rubatto, D., 2002, Zircon trace element geochemistry: partitioning with garnet and the 779
link between U‐Pb ages and metamorphism: Chemical Geology, v. 184, p. 123‐138. 780
Rubatto, D., Williams, I., Buck, I., 2001, Zircon and monazite response to prograde 781
metamorphism in the Reynolds Range, central Australia, Contrib. Mineral. Petrol., v. 782
140, p. 458‐468. 783
Saleeby, J.B., 2000, Geochronologic investigations along the Alexander‐Taku terrane 784
boundary, southern Revillagigedo Island to Cape Fox areas, southeast Alaska, in: Stowell, 785
H.H., McClelland, W.C., Eds., tectonics of the Coast Mountains, Southeastern Alaska and 786
British Columbia. Geological Society of America Special Paper 343, p.107‐144. 30
787
Saleeby, J.B., and Rubin, C.M., 1989, The western margin of the Coast Plutonic Complex 788
(CPC) in southernmost SE Alaska: Geological Society of America, Abstracts with 789
Programs, v. 21, p.139. 790
Saleeby, J.B., and Rubin, C.M., 1990, The east Behm gneiss complex (southern southeast 791
Alaska) and some insights into basement tectonics along the Insular suture belt: 792
Geological Association of Canada, Program with Abstracts, v. 15: A116. 793
Samson, S.D., 1990, Nd and Sr isotopic characterization of the Wrangellia, Alexander, 794
Stikine, Taku, and Yukon crystalline terranes of the Canadian Cordillera: PhD. 795
Dissertation, University of Arizona, Tucson. 796
Samson, S.D., Patchett, P.J., Gehrels, G.E., Anderson, R.G., 1990a, Nd and Sr isotopic 797
characterization of the Wrangellia terrane and implications for crustal growth of the 798
Canadian Cordillera: Journal of Geology, v. 98, p. 749‐762 799
Soja, C.M., 1994, Significance of Silurian stromatolite‐sphinctozoan reefs: Geology, v. 22, 800
p. 355–358. 801
Soja, C.M., and Kruitkov, L., 2008, Provenance, depositional setting, and tectonic 802
implications of Silurian polymictic conglomerates in Alaska’s Alexander terrane, in: 803
Blodgett, R., Stanley, G., eds., The terrane puzzle: New perspectives on paleontology 804
and stratigraphy from the North American Cordillera. Geological Society of America 805
Special Paper 442, p. 63‐75. 806
Stacey, J.S., and Kramers, J.D., 1975, Approximation of terrestrial lead isotope evolution 807
by a two‐stage model. Earth and Planetary Science Letters, v. 26, p. 207‐221. 808
Stevenson, R.K., Whittaker, S., and Mountjoy, E.W., 2000, Geochemical and Nd isotopic 809
evidence for sedimentary‐source changes in the Devonian miogeocline of the southern 810
Canadian Cordillera: Geological Society of America Bulletin, v. 112 (4), p. 531‐539. 811
Stowell, H.H., and Hooper, R.J., 1990, Structural development of the western 812
metamorphic belt adjacent to the Coast Plutonic Complex, evidence from Holkham Bay: 31
813
Tectonics, v. 9, p. 391‐407. 814
Templelman‐Kluitt, D.J., 1976, The Yukon crystalline terrane: Enigma in the Canadian 815
Cordillera: Geological Society of America Bulletin, v. 87, p. 1343‐1357. 816
Tochilin, C.J., Gehrels, G.E., Nelson, J.A., Mahoney, B.M., in press, U‐Pb and Hf isotope 817
analysis of detrital zircons in quartzites of the Banks Island Assemblage to identify 818
potential source terranes and origins: Lithosphere. 819
Vervoort, J.D., and Patchett, P.J., 1996, Behavior of hafnium and neodymium isotopes in 820
the crust: Constraints from crustally derived granites: Geochimica et Cosmochimica 821
Acta, v. 60 (19), p. 3717‐3733. 822
Vervoort, J.D., and Blichert‐Toft, J., 1999, Evolution of the depleted mantle: Hf isotope 823
evidence from juvenile rocks through time: Geochimica et Cosmochimica Acta, v. 63, p. 824
533‐556. 825
Vervoort, J.D., Patchett, P.J., Blichert‐Toft, J., and Albarede, F., 1999, Relationships 826
between Lu‐Hf and Sm‐Nd isotopic systems in the global sedimentary system: Earth and 827
Planetary Science Letters, v. 168, p. 79‐99. 828
Williams, I., 2001, Response of detrital zircon and monazite and their U‐Pb isotopic 829
systems, to regional metamorphism and host‐rock partial melting, Cooma complex, 830
southeastern Australia, Australian Journal of Earth Science, v. 48, p. 557‐580. 831
Wooden,J.L.,Barth,A.P.,andMueller,P.A.,2012,Crustalgrowthandtectonic
832
evolutionoftheMojavecrustalprovince:Insightsfromhafniumisotopesystematics
833
inzircons:Lithosphere,v.(10.1130/L218.1)
834
835
FIGURE CAPTIONS 836
Figure 1. Generalized terrane map of southeastern Alaska, including the Yukon‐Tanana 837
Coast Mountains project area and 2012 geochronology samples (adapted from Wheeler 838
and McFeely, 1991). Regional project outlines are as follows: A) Thorne Arm to Carroll 32
839
Inlet, B) Bradfield Canal to Thomas Bay, C) Port Houghton, and D) Tracy Arm to Port 840
Snettisham. 841
842
Figure 2. Schematic stratigraphic section of the Yukon‐Tanana terrane, Coast Mountains 843
section, southeast Alaska (adapted from Gehrels et al., 1992). Stratigraphic position of 844
many of the YTT samples is based on geochronolgical results presented in this study. 845
Sample locations are indicated by assemblage, with approximate stratigraphic position 846
noted by red star where known. Tracy Arm Assemblage samples only show approximate 847
relative position due to uncertain stratigraphic position of these samples. 848
Representative outcrop photographs as indicated: A) 12MP38, Port Houghton 849
Assemblage (PHA), pebble conglomerate; B) 12MP25, PHA, quartzite, highly folded 850
quartzite; C) 12MP08, Endicott Arm Assemblage (EAA), metarhyolite; D) 12MP19, EAA, 851
Quartz‐eye rhyolite porphyry, pen indicating 7mm diameter “bluish” quartz eye; E) 852
12MP41, Tracy Arm Assemblage (TAA), orthoquartzite; F) 12MP11, TAA typical folding 853
within TAA quartzite 854
855
Figure 3. Lower portion: Composite normalized U‐Pb age distribution diagrams for the 856
three Yukon‐Tanana Coast Mountains Assemblages (Tracy Arm, Endicott Arm, and Port 857
Houghton), and three proposed Alexander terrane samples. N= number of samples and 858
n= total number of U‐Pb laser analyses in each respective distribution. Upper portion: 859
Hf isotopic data from YTT Coast Mountains (this study). Color indicates specific YTT 860
assemblage. Average age uncertainty of all analyses shown is 1.2 epsilon units (at 1‐
861
sigma). Average crustal evolution slope is based upon a 176Lu/177Hf ratio of 0.0093 862
(Vervoort and Patchett, 1996; Amelin et al., 2000; Bahlburg et al., 2011. 863
864
Figure 4. Lower portion: 250‐600 Ma only composite normalized U‐Pb age distribution 865
diagrams for the Endicott Arm and Port Houghton Assemblages, and comparisons to 866
Alexander terrane samples. N= number of samples and n= total number of U‐Pb laser 867
analyses in each respective distribution. Upper portion: 250‐600 Ma only Hf isotopic 33
868
data from Endicott Arm and Port Houghton Assemblages, in comparison to Alexander 869
terrane (this study and published reference data). Average age uncertainty of all 870
analyses shown is 1.2 epsilon units (at 1‐sigma). Average crustal evolution slope is 871
based upon a 176Lu/177Hf ratio of 0.0093 (Vervoort and Patchett, 1996; Amelin et al., 872
2000; Bahlburg et al., 2011. 873
874
Figure 5. Composite normalized U‐Pb age distribution diagrams for zircon grains from 875
Yukon‐Tanana terrane (YTT), Alexander terrane (AXT), and North American miogeoclinal 876
(NAM) transects. YTT reference data from (Gehrels et al., 1992; Gehrels and Kapp, 877
1998; Gehrels and Boghossian, 2000; Gehrels, 2000b, 2001; Dusel‐Bacon et al., 2003; 878
Dusel‐Bacon et al.,2013; Colpron et al., 2006). AXT reference includes data from: Banks 879
Island Assemblage (Tochilin et al., in press), and Saint Elias Mountains (Berranek et al, 880
2013 a, b). NAM reference includes data from Gehrels et al., 1995; Gehrels and Pecha, 881
in press; Wooden et al., 2012. Miogeoclinal transects for Alaska & northern British 882
Columbia, and California & Sonora are grouped together for comparison, respectively. 883
Where indicated (i.e. 8x on YTT distribution) the main peak was reduced by the factor 884
shown for comparison purposes only. 885
886
Figure 6. Hf isotopic data from YTT Coast Mountains (this study) overlain on North 887
American miogeoclinal Hf data. Miogeoclinal data from (Gehrels et al., 1995; Gehrels 888
and Pecha, in press; Wooden et al., 2012 (California only) A) Alaska and northern British 889
Columbia transects combined, B) Southern British Columbia transect, C) Nevada 890
transect, D) California and Sonora transects combined. 891
34
892
35
893
36
894
37
895
38
896
39
897
40
DR-3 Table 1. P-values, Kolmogorov-Smirnoff (K-S) statistical comparisons
Analysis run on: Monday, Nov 25, 2013 @ 12:38:21 PM. Version: 1.0.
12MP03
12MP04
12MP05
12MP06
12MP07
12MP08
12MP09
12MP11
12MP12
12MP13
12MP14
12MP15
12MP16
12MP17
12MP18
12MP19
12MP20
12MP23
12MP24
12MP25
12MP33
12MP38
12MP39
12MP40
12MP41
K-S P-values using error in the CDF
12MP03
12MP04
12MP05
12MP06
0.000
0.000
0.000
0.000
0.002
0.000
0.000
0.002
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.006
0.973
0.000
0.000
0.000
0.000
0.000
0.000
0.381
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.006
0.006
0.006
0.010
0.007
0.023
0.089
0.047
0.000
0.942
0.513
0.000
0.000
0.060
0.958
0.000
0.000
0.000
0.000
0.033
0.000
0.000
0.000
0.016
0.000
0.000
0.000
0.102
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.007
0.000
0.000
0.000
0.000
0.000
12MP07
0.000
0.000
0.000
0.006
0.000
0.074
0.000
0.000
0.000
0.000
0.000
0.000
0.006
0.006
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
12MP08
12MP09
0.973
0.000
0.000
0.000
0.000
0.000
0.000
0.381
0.000
0.074
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.009
0.009
0.013
0.009
0.001
0.000
0.000
0.000
0.000
0.003
0.000
0.001
0.000
0.016
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
12MP11
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.009
0.325
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
12MP12
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.272
0.000
0.000
0.000
0.978
0.010
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
12MP13
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.272
0.000
0.000
0.000
1.000
0.014
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
12MP14
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.251
0.257
0.011
0.176
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
12MP15
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.251
0.002
0.009
0.217
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
12MP16
12MP17 12MP18 12MP19 12MP20
0.000
0.006
0.007
0.000
0.000
0.000
0.006
0.023
0.942
0.060
0.000
0.006
0.089
0.513
0.958
0.000
0.010
0.047
0.000
0.000
0.000
0.006
0.006
0.000
0.000
0.000
0.009
0.013
0.001
0.000
0.000
0.009
0.009
0.000
0.000
0.000
0.009
0.325
0.000
0.000
0.000
0.978
0.010
0.000
0.000
0.000
1.000
0.014
0.000
0.000
0.257
0.011
0.176
0.000
0.000
0.002
0.009
0.217
0.000
0.000
0.007
0.139
0.000
0.000
0.007
0.100
0.014
0.012
0.139
0.100
0.150
0.219
0.000
0.014
0.150
0.506
0.000
0.012
0.219
0.506
0.000
0.108
0.006
0.000
0.000
0.000
0.169
0.007
0.000
0.000
0.000
0.075
0.009
0.000
0.000
0.000
0.011
0.008
0.000
0.000
0.000
0.013
0.883
0.000
0.000
0.000
0.436
0.157
0.000
0.000
0.000
0.006
0.351
0.738
0.467
0.000
0.028
0.015
0.000
0.000
12MP23 12MP24 12MP25 12MP33 12MP38 12MP39 12MP40 12MP41
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.007
0.000
0.033
0.016
0.102
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.003
0.001
0.016
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.108
0.169
0.075
0.011
0.013
0.436
0.006
0.028
0.006
0.007
0.009
0.008
0.883
0.157
0.351
0.015
0.000
0.000
0.000
0.000
0.000
0.000
0.738
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.467
0.000
0.986
0.899
0.000
0.000
0.000
0.000
0.000
0.986
0.614
0.000
0.000
0.000
0.000
0.000
0.899
0.614
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.217
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0.217
0.000
0.000
0.000
Cathodoluminescene images of representative zircons from SEAK geochronologic samples, incl
luding U-Pb (white) and Hf (yellow) spot locations where applicable
DR-2 Supplemental Text table #1. U-Pb geochronologic analyses.
Isotope ratios
Analysis
U
(ppm)
206Pb
204Pb
U/Th
206Pb*
207Pb*
±
(%)
207Pb*
235U*
±
(%)
12MP03 Yukon-Tanana, Endicott Arm Assemblage, quartz-eye rhyolite (Degree Decimal: 55.33162
12MP03-95
788
20624
1.2 18.0262
1.1
0.3783
3.9
12MP03-81
631
14865
1.4 18.2957
1.6
0.4150
4.0
12MP03-39
227
13507
2.6 18.7332
3.8
0.4168
4.3
12MP03-37
219
16794
2.5 17.9397
1.7
0.4416
4.7
12MP03-46
421
46682
1.4 18.1754
2.6
0.4399
6.8
12MP03-65
298
3885
2.0 18.0821
3.5
0.4429
4.9
12MP03-20
363
10903
1.7 18.0020
2.2
0.4510
3.6
12MP03-79
298
94629
2.2 18.4241
2.3
0.4450
2.7
12MP03-106
210
4440
2.4 18.0417
4.6
0.4605
4.9
12MP03-45
229
84365
2.1 18.7098
4.3
0.4484
4.6
12MP03-4
245
42189
2.5 17.9178
2.3
0.4698
2.9
12MP03-22
366
25628
1.9 17.8262
4.1
0.4731
5.4
12MP03-3
317
57324
1.6 17.9502
3.1
0.4709
3.4
12MP03-7
300
6417
1.6 17.4301
3.9
0.4874
4.5
12MP03-108
297
46380
1.6 18.2118
2.0
0.4703
2.3
12MP03-58
249
57527
1.7 18.5253
3.1
0.4637
3.6
12MP03-74
233
27239
2.0 18.0774
2.8
0.4759
3.5
12MP03-105
293
14973
2.0 18.0633
2.6
0.4766
2.8
12MP03-78
335
54431
1.9 18.1453
2.2
0.4748
2.8
12MP03-61
489
24179
1.4 18.0053
1.6
0.4785
2.6
12MP03-5
430
18336
1.2 18.1850
1.3
0.4753
4.8
12MP03-40
444
27743
1.6 18.0977
1.4
0.4778
4.7
12MP03-68
386
90998
1.6 18.0617
1.6
0.4798
3.7
12MP03-60
263
51210
2.1 18.4018
2.5
0.4719
2.8
12MP03-33
478
41187
1.5 18.1050
1.5
0.4803
2.2
12MP03-97
403
69043
1.6 17.9680
2.1
0.4844
3.2
12MP03-94
449
13113
1.2 17.9250
1.4
0.4856
2.3
12MP03-9
288
126518
2.4 18.1195
2.7
0.4807
3.2
12MP03-30
248
43331
2.1 17.9851
3.2
0.4845
4.3
12MP03-43
673
116827
1.0 18.0959
1.0
0.4817
1.5
12MP03-82
180
9639
3.1 17.6210
5.0
0.4947
5.2
12MP03-13
178
53579
2.2 18.0437
7.2
0.4834
7.2
12MP03-8
443
132303
1.4 18.1254
2.1
0.4822
2.3
12MP03-38
313
44126
1.8 17.8536
3.5
0.4896
3.7
12MP03-23
264
77072
2.1 17.9404
2.1
0.4872
2.4
12MP03-51
243
6918
2.2 17.4241
4.1
0.5020
4.4
12MP03-69
352
268268
1.5 18.1300
2.1
0.4827
2.4
12MP03-56
243
41860
1.5 18.4337
4.2
0.4766
8.4
12MP03-54
234
34442
2.9 18.0193
2.1
0.4881
2.6
12MP03-72
344
86105
1.7 18.1419
1.8
0.4850
2.1
12MP03-102
262
79960
1.8 17.9308
1.9
0.4910
2.1
12MP03-110
173
23133
2.6 16.9149
4.1
0.5205
4.5
12MP03-48
185
124073
2.5 18.2020
4.4
0.4843
5.0
12MP03-16
260
64369
2.1 17.7801
2.1
0.4958
2.4
12MP03-18
344
12335
1.8 17.7028
2.7
0.4981
3.1
12MP03-49
12MP03-92
12MP03-36
12MP03-107
12MP03-67
12MP03-19
12MP03-93
12MP03-77
12MP03-42
12MP03-103
12MP03-104
12MP03-44
12MP03-84
12MP03-29
12MP03-89
12MP03-32
12MP03-109
12MP03-57
12MP03-14
12MP03-25
12MP03-12
12MP03-87
12MP03-75
12MP03-6
12MP03-86
12MP03-50
12MP03-85
12MP03-101
12MP03-28
12MP03-24
12MP03-17
12MP03-34
12MP03-55
12MP03-62
12MP03-100
12MP03-11
12MP03-96
12MP03-27
12MP03-91
12MP03-90
12MP03-41
12MP03-66
12MP03-35
12MP03-71
12MP03-21
12MP03-83
12MP03-52
12MP03-88
12MP03-70
12MP03-53
12MP03-80
12MP03-2
329
271
301
722
260
300
299
326
224
166
356
269
196
254
398
352
290
259
334
206
258
256
325
320
231
278
310
225
162
207
300
363
229
392
541
260
271
276
245
291
238
371
242
280
323
238
365
142
233
327
278
255
26589
64847
114285
92095
37827
59737
58484
69491
57352
44553
96706
40441
51547
73192
26637
167869
117151
27107
81721
52744
7451
61793
14663
34534
27561
60048
91045
56690
8647
53647
14341
76963
54433
7714
55424
51964
70411
47343
85345
51718
58844
45952
52683
47301
34683
100261
92771
21889
42230
150489
78398
2470
1.7
2.2
1.7
1.2
2.1
1.7
1.6
1.8
2.2
2.2
1.8
2.7
2.7
2.2
1.2
1.7
1.9
2.2
1.7
2.1
2.2
2.2
1.9
1.5
2.4
1.9
1.7
2.2
3.2
2.2
2.0
1.4
2.1
1.4
1.7
2.1
2.1
1.9
2.4
1.9
2.5
1.5
2.2
1.7
1.7
2.6
1.5
3.0
2.1
1.3
2.0
1.9
18.2797
18.3923
18.2536
18.1561
18.1364
18.1038
18.2126
18.3943
17.9465
17.8671
18.3345
18.0878
18.5171
17.9069
17.6460
17.9734
18.3184
18.4121
18.1705
18.1437
17.5184
18.4814
17.9018
18.0169
17.3093
17.9478
18.2257
18.2134
18.4395
18.4288
18.0335
17.9611
18.3889
17.6425
18.2275
18.2241
18.2267
18.2429
18.1906
17.7841
18.1471
18.4011
18.1450
18.5654
18.3553
18.4673
17.8750
18.5126
18.2175
17.8600
18.0655
17.6135
3.3
3.1
1.4
1.1
2.9
1.8
2.2
1.3
2.6
5.3
1.7
1.7
2.5
2.5
1.8
1.5
2.5
2.4
2.1
4.9
4.1
3.1
2.4
2.9
9.8
2.2
1.2
1.6
4.0
4.0
3.0
2.4
2.3
3.7
0.9
1.7
1.8
2.2
2.5
2.6
2.0
1.0
2.7
2.2
1.7
2.9
1.2
5.7
3.5
2.2
3.0
4.3
0.4829
0.4801
0.4838
0.4875
0.4883
0.4893
0.4864
0.4819
0.4941
0.4971
0.4846
0.4914
0.4801
0.4966
0.5041
0.4950
0.4862
0.4838
0.4908
0.4919
0.5099
0.4833
0.4992
0.4963
0.5170
0.4989
0.4913
0.4918
0.4858
0.4863
0.4970
0.4991
0.4876
0.5083
0.4921
0.4925
0.4926
0.4928
0.4944
0.5068
0.4971
0.4911
0.4983
0.4876
0.4943
0.4914
0.5096
0.4923
0.5003
0.5115
0.5058
0.5199
3.3
3.4
1.7
1.3
3.0
1.9
2.7
3.9
3.0
5.4
2.0
1.9
3.2
2.6
2.2
2.2
2.8
2.8
4.2
4.9
5.7
3.6
3.5
3.1
10.1
2.6
1.8
2.1
4.2
4.1
3.7
2.6
2.4
3.8
2.5
1.8
2.0
2.7
2.7
3.3
4.0
2.0
2.7
2.4
1.9
3.1
1.7
5.8
3.7
3.8
3.3
4.7
12MP03-26
12MP03-98
12MP03-63
12MP03-47
12MP03-73
12MP03-1
243
259
177
235
138
175
42903
41210
23133
74669
24847
49342
1.8
1.9
2.2
2.1
2.5
2.6
18.3764
17.9912
18.6515
17.4082
18.3232
17.9196
3.1
4.1
4.4
3.9
6.4
3.6
0.4984
0.5104
0.4924
0.5365
0.5135
0.5463
3.2
4.4
4.9
7.1
8.6
3.7
12MP04; Yukon-Tanana, Port Houghton Assemblage, chippy breccia (Degree Decimal: 55.33634,
1696
70189
0.9 18.5098
0.5
0.3251
1.3
12MP04-21
12MP04-22
848
51360
1.2 18.2087
1.0
0.3883
4.8
12MP04-29
919
136559
1.0 18.3155
0.6
0.4071
9.7
12MP04-24
1377
86348
1.9 18.4907
0.4
0.4061
1.8
12MP04-01
63
18546
2.7 18.1129
10.2
0.4230
11.2
12MP04-28
987
197458
2.5 18.3375
0.7
0.4262
1.1
12MP04-97
199
35000
1.2 18.4339
3.3
0.4367
6.0
12MP04-73
167
38488
1.4 18.4312
3.0
0.4375
3.5
12MP04-04
85
13246
1.5 18.9804
8.4
0.4257
8.5
12MP04-98
119
66273
1.4 18.0545
3.3
0.4494
4.1
12MP04-18
81
17738
1.6 17.9939
4.6
0.4512
4.8
12MP04-38
71
29123
2.7 19.5756
7.8
0.4162
8.1
12MP04-09
106
16268
1.6 19.6055
5.1
0.4161
5.4
12MP04-65
48
13751
2.0 18.0183
8.2
0.4530
9.8
12MP04-32
91
20534
2.3 17.7055
3.8
0.4613
5.6
12MP04-49
175
37545
2.2 18.2110
3.8
0.4489
3.9
12MP04-15
76
27395
1.8 17.6955
7.8
0.4627
8.1
12MP04-52
149
23560
1.9 18.0370
4.1
0.4541
4.6
12MP04-88
76
28521
2.0 18.8265
6.7
0.4353
7.2
12MP04-34
65
18851
1.8 19.0987
10.6
0.4291
10.7
12MP04-74
84
18978
2.1 18.8489
6.0
0.4352
7.0
12MP04-36
156
29677
2.3 18.5394
3.8
0.4428
4.1
12MP04-35
93
22343
2.0 19.1608
4.9
0.4289
5.2
12MP04-78
63
12095
2.8 18.1886
7.7
0.4519
8.2
12MP04-31
109
19924
2.5 19.1195
4.6
0.4301
5.0
12MP04-19
106
19774
2.5 18.3348
3.6
0.4488
3.7
12MP04-94
619
112161
1.4 18.1824
0.7
0.4526
1.4
12MP04-06
367
103567
1.9 18.3508
2.8
0.4485
3.3
12MP04-99
118
41791
2.0 17.5972
5.9
0.4678
6.0
12MP04-25
600
151914
0.9 18.3055
0.6
0.4510
0.9
12MP04-63
217
45925
1.3 18.6441
2.4
0.4428
3.2
12MP04-07
101
32001
1.9 19.1668
6.4
0.4309
6.6
12MP04-41
77
15845
2.6 18.7922
7.1
0.4400
7.3
12MP04-33
216
45082
2.5 18.8026
4.1
0.4403
4.1
12MP04-82
76
22048
2.2 19.5610
6.7
0.4236
7.3
12MP04-02
269
96958
1.7 18.4963
1.7
0.4480
2.2
12MP04-42
105
37864
1.7 17.8385
4.5
0.4647
5.3
12MP04-84
37
6295
2.9 17.6450
16.4
0.4702
16.7
12MP04-69
85
25062
2.7 18.7066
5.4
0.4441
5.7
12MP04-87
125
23648
1.6 17.9006
3.9
0.4643
4.2
12MP04-66
384
92423
1.2 18.4741
1.8
0.4500
2.0
12MP04-80
75
26899
1.9 18.9358
5.9
0.4392
6.1
12MP04-48
158
53744
1.5 18.8695
5.3
0.4408
5.8
12MP04-13
204
43296
1.2 18.4834
1.7
0.4501
2.5
12MP04-55
12MP04-17
12MP04-12
12MP04-37
12MP04-30
12MP04-58
12MP04-23
12MP04-43
12MP04-27
12MP04-46
12MP04-100
12MP04-60
12MP04-72
12MP04-79
12MP04-57
12MP04-05
12MP04-81
12MP04-50
12MP04-10
12MP04-86
12MP04-85
12MP04-61
12MP04-68
12MP04-70
12MP04-03
12MP04-08
12MP04-71
12MP04-56
12MP04-14
12MP04-20
12MP04-53
12MP04-90
12MP04-64
12MP04-26
12MP04-45
12MP04-39
12MP04-44
12MP04-62
12MP04-96
12MP04-59
12MP04-54
12MP04-11
12MP04-40
12MP04-89
12MP04-93
12MP04-95
12MP04-47
12MP04-91
12MP04-77
12MP04-92
12MP04-75
12MP04-83
757
906
107
900
736
90
81
508
75
435
70
220
107
210
402
596
655
173
61
379
555
84
98
869
973
113
364
47
625
136
442
73
740
603
193
869
601
397
456
95
724
489
802
647
242
54
301
273
138
573
426
42
140494
245475
103585
182713
208600
22212
27647
79022
19594
105813
17452
46562
34120
39029
83388
310251
240851
40019
50874
80996
152786
16445
15658
546171
397384
59260
38516
21547
18631
54405
132015
24548
307456
285133
75365
175733
132362
53053
173059
28782
32423
117794
153112
354029
56002
7985
105330
94600
69566
148275
109311
10914
1.4
1.2
1.9
1.2
1.2
1.8
1.9
0.9
2.6
2.1
2.8
2.0
2.0
1.8
1.6
1.1
1.5
1.9
2.2
1.6
1.3
2.3
2.0
1.2
1.5
2.9
1.3
2.8
1.7
1.9
1.3
2.2
1.1
1.5
2.3
0.9
1.3
1.3
1.4
2.2
1.3
1.6
1.3
2.0
1.8
2.7
0.8
1.7
1.9
1.2
1.4
2.5
18.3335
18.3074
17.8809
18.3027
18.5156
18.2738
18.0984
18.1626
18.3384
18.3167
17.8045
18.2592
18.3655
18.3335
18.3553
18.4263
18.2979
18.7195
19.7891
18.3302
18.3565
17.7328
19.2103
18.2365
18.3334
18.5843
18.5315
19.8786
18.3848
18.6482
18.2079
18.5908
18.4204
18.3878
18.2089
18.2970
18.3142
18.3453
18.3348
17.8966
18.1410
18.3900
18.3364
18.4093
18.3773
18.2561
18.3276
18.3408
18.2117
18.2240
18.3090
19.0920
1.0
0.6
6.6
0.7
0.7
7.5
5.6
0.8
5.4
1.3
5.3
2.0
4.5
4.5
0.8
0.8
1.0
3.5
7.0
1.5
1.0
7.4
5.5
0.9
0.6
5.2
2.1
11.1
1.2
3.9
1.2
9.7
0.9
0.7
3.9
0.7
0.7
0.5
1.5
6.4
1.4
1.5
0.7
0.6
2.8
7.1
1.0
1.8
5.5
1.0
0.8
11.3
0.4538
0.4545
0.4654
0.4549
0.4496
0.4556
0.4604
0.4589
0.4548
0.4557
0.4690
0.4574
0.4548
0.4556
0.4552
0.4539
0.4571
0.4474
0.4233
0.4571
0.4567
0.4730
0.4370
0.4603
0.4580
0.4520
0.4535
0.4228
0.4577
0.4513
0.4623
0.4529
0.4577
0.4587
0.4633
0.4615
0.4617
0.4613
0.4615
0.4731
0.4670
0.4609
0.4624
0.4609
0.4624
0.4657
0.4642
0.4644
0.4678
0.4686
0.4678
0.4493
1.4
1.1
6.8
2.2
2.6
7.6
6.6
2.5
6.0
1.5
5.7
2.4
4.9
5.3
1.5
2.0
1.6
3.6
7.3
2.0
1.4
7.6
6.2
1.3
1.2
5.4
4.3
11.4
1.8
4.3
2.1
10.0
1.5
2.0
4.0
1.1
1.3
1.2
1.8
7.1
1.5
2.0
3.3
1.6
3.2
8.3
1.5
2.4
6.0
1.6
1.4
12.2
12MP04-76
12MP04-51
12MP04-67
78
368
64
52398
108867
23979
2.9
1.4
2.9
18.6512
18.4061
18.6723
8.3
1.5
6.3
0.4610
0.4673
0.4630
8.5
4.5
6.8
12MP05; Yukon-Tanana, Port Houghton Assemblage, conglomerate (Degree Decimal: 55.29912, 1
916
73952
0.9 18.6421
1.0
0.3384
1.7
12MP05-62
12MP05-6
421
26244
1.2 18.5537
2.4
0.3575
5.1
12MP05-103
512
111148
1.0 18.7918
1.1
0.3675
3.1
12MP05-67
265
50566
0.6 18.4752
3.8
0.3859
6.4
12MP05-24
538
111169
1.0 18.6037
1.8
0.3847
6.6
12MP05-78
235
80078
1.6 18.6504
2.9
0.3862
5.0
12MP05-61
317
72701
1.3 18.4297
3.3
0.3949
4.6
12MP05-59
546
143478
1.0 18.5968
1.6
0.3947
4.5
12MP05-19
209
29045
1.7 18.4242
2.8
0.4109
3.9
12MP05-11
519
53269
1.1 18.4769
2.0
0.4130
2.2
12MP05-38
213
34367
1.1 18.0698
3.9
0.4260
4.2
12MP05-29
307
85371
1.5 18.4277
2.7
0.4209
3.5
12MP05-12
245
53523
1.4 18.7375
2.7
0.4145
4.0
12MP05-18
288
48658
1.5 18.5939
2.7
0.4179
3.0
12MP05-90
441
54000
1.1 18.2278
2.1
0.4268
2.7
12MP05-91
384
71668
1.4 18.3634
1.7
0.4268
2.0
12MP05-68
241
46885
1.6 18.2397
4.5
0.4301
6.8
12MP05-81
244
42964
0.9 17.7676
5.0
0.4420
8.0
12MP05-95
186
43349
1.8 18.4482
3.1
0.4260
3.8
12MP05-26
201
38993
1.8 18.8766
4.5
0.4190
4.6
12MP05-9
306
48541
1.4 18.3140
2.0
0.4333
2.5
12MP05-1
144
26985
1.4 19.2592
7.5
0.4136
7.7
12MP05-8
289
81917
1.4 18.7225
2.6
0.4255
4.1
12MP05-13
257
60819
0.9 18.3073
3.6
0.4365
3.8
12MP05-34
614
114162
1.1 18.4402
1.5
0.4355
1.7
12MP05-10
274
96594
1.3 18.6192
3.9
0.4319
5.0
12MP05-47
258
83352
0.9 18.5273
3.1
0.4341
3.2
12MP05-72
184
49529
1.4 18.4227
4.9
0.4370
4.9
12MP05-105
817
100022
0.9 18.4568
0.9
0.4364
2.6
12MP05-28
275
50446
1.5 18.2699
1.8
0.4410
2.4
12MP05-25
341
80063
1.3 18.4475
1.9
0.4370
2.2
12MP05-7
232
50862
1.7 18.8086
2.1
0.4289
2.4
12MP05-65
322
85074
1.0 18.4426
3.3
0.4378
7.2
12MP05-60
272
60987
1.2 18.4780
3.4
0.4376
3.7
12MP05-16
216
14636
1.5 17.4234
6.1
0.4641
6.2
12MP05-98
241
52192
1.7 18.4989
2.5
0.4374
2.6
12MP05-49
532
127025
1.3 18.5034
1.2
0.4376
1.4
12MP05-70
366
63255
1.2 18.4796
2.8
0.4382
2.9
12MP05-82
162
54310
1.6 19.3553
3.5
0.4186
3.7
12MP05-44
514
105898
1.0 18.3218
1.9
0.4425
2.4
12MP05-17
269
40693
1.3 18.5123
1.6
0.4380
2.5
12MP05-30
300
44759
1.8 17.9333
7.3
0.4524
8.1
12MP05-79
277
59517
1.6 18.1678
1.4
0.4468
2.5
12MP05-23
179
44813
2.0 18.8105
5.3
0.4317
5.5
12MP05-33
151
26793
1.8 18.5676
3.8
0.4375
3.8
12MP05-36
172
48880
1.5 17.8060
3.0
0.4565
3.9
12MP05-76
246
65647
1.7 18.4755
2.1
0.4403
2.3
12MP05-101
12MP05-97
12MP05-21
12MP05-80
12MP05-88
12MP05-77
12MP05-3
12MP05-96
12MP05-4
12MP05-75
12MP05-32
12MP05-2
12MP05-56
12MP05-84
12MP05-74
12MP05-46
12MP05-86
12MP05-89
12MP05-5
12MP05-43
12MP05-100
12MP05-14
12MP05-42
12MP05-92
12MP05-55
12MP05-66
12MP05-41
12MP05-27
12MP05-87
12MP05-85
12MP05-57
12MP05-94
12MP05-71
12MP05-93
12MP05-58
12MP05-54
12MP05-40
12MP05-50
12MP05-99
12MP05-64
12MP05-45
12MP05-20
12MP05-73
12MP05-83
12MP05-102
12MP05-104
12MP05-35
12MP05-31
12MP05-52
12MP05-51
12MP05-22
12MP05-37
364
213
235
314
319
687
127
176
147
251
298
242
118
108
184
310
251
258
397
214
135
145
381
215
189
169
168
291
275
243
286
149
109
203
194
154
272
268
65
246
152
264
374
137
194
213
197
203
205
226
262
340
106445
79596
51366
109008
59518
151161
30825
33772
45783
75868
62144
53800
42513
41050
32353
55309
46765
45598
78219
79861
22399
65454
53721
48524
46665
27946
38522
49569
90427
56251
93797
78482
16989
61105
37222
23131
53871
37774
8710
64049
22107
71151
88766
50642
23197
49250
52019
138219
70165
76292
59241
126758
1.4
1.7
1.6
1.3
0.9
1.9
1.3
1.9
1.5
1.8
1.0
1.5
1.7
1.6
1.6
1.4
0.7
1.6
0.9
1.6
1.7
1.3
1.2
1.7
1.5
1.7
1.6
1.3
1.5
1.7
1.3
1.1
1.9
1.6
1.5
2.1
1.6
1.0
2.4
1.3
1.4
1.9
1.1
2.1
1.4
1.4
1.9
3.0
1.6
1.3
2.4
1.3
18.4452
18.4566
18.7648
18.2794
18.1153
18.4278
18.3154
18.5030
19.3229
18.7631
18.5390
18.5081
18.2696
18.5641
18.5066
18.5581
18.5835
18.2057
18.3855
18.3370
19.1164
17.8898
18.1459
17.9100
18.3547
18.7980
18.4573
18.7555
18.4795
18.5564
18.7304
18.1492
17.8742
18.6737
18.2150
18.2639
18.4067
18.1214
19.5398
18.5404
18.1082
18.4471
18.3248
18.1840
18.0513
18.7248
18.2825
18.2060
18.4057
18.9206
18.1443
18.5036
2.1
3.1
3.0
2.8
4.3
1.3
3.9
3.6
3.0
3.1
3.1
2.7
5.6
7.9
3.7
2.3
2.9
1.5
1.5
3.6
5.4
3.5
1.6
3.3
3.6
4.2
3.3
2.7
2.5
3.3
3.3
3.7
7.1
2.8
3.2
4.8
3.0
3.3
12.1
3.8
5.7
2.6
1.5
6.7
4.6
2.9
3.7
4.2
4.4
3.5
1.5
2.9
0.4410
0.4410
0.4338
0.4457
0.4500
0.4424
0.4453
0.4415
0.4228
0.4356
0.4413
0.4420
0.4478
0.4408
0.4423
0.4414
0.4411
0.4505
0.4461
0.4475
0.4295
0.4591
0.4527
0.4589
0.4478
0.4375
0.4459
0.4389
0.4455
0.4437
0.4397
0.4540
0.4613
0.4418
0.4532
0.4522
0.4488
0.4561
0.4234
0.4472
0.4589
0.4509
0.4546
0.4584
0.4621
0.4455
0.4568
0.4604
0.4581
0.4477
0.4672
0.4588
3.4
3.5
3.2
3.0
4.4
1.8
4.5
3.8
3.4
3.2
3.4
2.8
6.0
8.2
3.8
2.9
3.1
1.8
2.2
4.1
5.6
4.4
1.8
3.5
3.8
4.3
3.7
2.8
2.9
3.4
3.5
4.2
7.3
3.0
3.6
5.2
4.0
3.4
12.6
4.0
5.7
2.6
2.0
6.9
4.8
3.2
4.2
5.2
4.8
3.6
1.8
3.0
12MP05-39
12MP05-63
12MP05-53
153
272
141
44197
7274
29273
1.4
1.0
1.9
18.3280
17.6518
18.4120
4.8
6.9
5.8
0.4790
0.5037
0.4942
5.1
10.0
5.9
12MP06; Yukon-Tanana, meta-trondjemite, (Degree Decimal: 55.43796, 131.32647)
12MP06-46C
84
5784
195.9 20.3748
2.0
0.0983
12MP06-38C
91
5002
108.5 20.0794
3.6
0.1012
12MP06-43C
2243
132909
13.5 17.8940
0.7
0.3300
12MP06-22C
318
106403
12.4 18.0942
0.8
0.4469
433
202260
1.2 18.0106
0.9
0.4572
12MP06-32R
12MP06-42C
167
39059
1.2 18.0237
1.0
0.4999
12MP06-30C
219
149698
2.0 17.9862
0.7
0.5129
12MP06-21R
140
73993
2.5 17.7577
0.6
0.5264
12MP06-29C
270
113231
1.6 17.8804
0.6
0.5293
12MP06-28C
132
50516
2.5 17.5580
6.4
0.5394
12MP06-27C
290
85210
1.9 17.9678
0.6
0.5314
12MP06-36C
337
293202
2.1 18.0097
0.8
0.5353
12MP06-35C
598
174411
1.6 17.9242
1.1
0.5380
12MP06-24C
175
44514
2.1 17.9037
0.7
0.5409
12MP06-31C
111
78489
2.3 18.0392
0.9
0.5425
12MP06-32C
98
39670
2.4 17.8005
0.9
0.5499
12MP06-26C
249
126794
2.6 18.0026
1.3
0.5445
12MP06-39C
120
38001
2.8 17.9145
1.2
0.5488
12MP06-34C
113
58350
2.2 17.9916
1.1
0.5467
12MP06-33C
223
80757
2.3 17.9251
0.9
0.5515
12MP06-21C
211
89824
2.0 17.7948
0.8
0.5559
12MP06-37C
173
97239
1.8 17.5639
0.9
0.5726
12MP06-40C
226
239421
2.4 17.8029
1.4
0.5707
12MP06-41C
197
55371
3.0 17.8790
0.7
0.5973
12MP06-25C
1662
413190
2.9 17.8054
2.2
0.6001
12MP06-44C
460
274499
3.2 17.9918
0.7
0.5978
2.8
3.8
4.9
5.0
4.9
1.3
3.7
1.7
1.5
6.9
1.2
2.5
4.8
1.3
2.8
1.9
4.0
1.4
2.0
1.7
2.0
1.1
3.2
2.6
6.7
4.3
12MP07; Yukon-Tanana, Endicott Arm Assemblage, fragmental volcanic, (Degree Decimal: 55.440
12MP07-23
64
22335
2.5 18.1294
6.9
0.4324
8.9
12MP07-24
852
93527
1.2 18.0538
1.0
0.4610
2.4
12MP07-73
501
95002
1.1 17.9202
1.2
0.4709
2.6
12MP07-96
213
58086
1.3 18.2582
1.5
0.4697
5.3
12MP07-14
417
91349
1.2 18.0008
0.7
0.4888
3.5
12MP07-76
364
59435
1.1 17.9405
1.1
0.4991
7.7
12MP07-79
113
22789
2.2 17.8952
4.6
0.5066
5.0
12MP07-59
310
138637
1.1 17.8435
1.4
0.5082
2.0
12MP07-78
461
274290
1.9 17.8428
1.7
0.5104
2.2
12MP07-80
286
76482
1.7 17.7928
1.1
0.5122
4.7
12MP07-20
85
30582
1.5 18.4248
3.6
0.4955
4.4
12MP07-28
154
38024
2.0 18.0999
3.7
0.5056
4.3
12MP07-18
53
16987
3.0 18.4873
7.6
0.4958
8.2
12MP07-87
85
48839
1.5 17.7489
4.8
0.5167
5.1
12MP07-22
75
18161
2.0 17.8930
5.9
0.5127
6.1
12MP07-26
111
51617
1.4 17.7754
4.4
0.5161
4.5
12MP07-19
73
32377
1.9 18.2302
4.9
0.5036
5.1
12MP07-33
289
45375
1.5 16.6622
9.7
0.5512
9.8
12MP07-04
51
12524
1.7 18.5093
7.4
0.4973
7.6
12MP07-01
12MP07-31
12MP07-42
12MP07-77
12MP07-93
12MP07-95
12MP07-92
12MP07-41
12MP07-38
12MP07-09
12MP07-06
12MP07-12
12MP07-36
12MP07-98
12MP07-56
12MP07-32
12MP07-85
12MP07-74
12MP07-90
12MP07-10
12MP07-46
12MP07-83
12MP07-60
12MP07-45
12MP07-17
12MP07-11
12MP07-30
12MP07-94
12MP07-43
12MP07-82
12MP07-44
12MP07-35
12MP07-13
12MP07-02
12MP07-71
12MP07-57
12MP07-37
12MP07-69
12MP07-91
12MP07-51
12MP07-29
12MP07-88
12MP07-07
12MP07-53
12MP07-72
12MP07-58
12MP07-47
12MP07-67
12MP07-84
12MP07-65
12MP07-21
12MP07-81
95
108
144
157
81
278
236
142
83
240
192
91
283
166
174
224
271
234
135
390
77
75
86
228
269
106
230
211
152
186
265
142
101
199
92
156
213
133
266
1013
136
99
115
280
190
211
174
297
320
137
332
192
31059
51498
31160
111452
49889
84901
74309
52011
41848
109305
71409
35814
89848
10302
85836
106778
78190
95366
65584
169626
37869
32916
35933
52484
84368
45335
53850
58490
46241
92940
22168
19885
47272
69695
34709
79153
73866
60988
36794
1224845
72899
45425
76868
73196
45017
92917
45328
90112
815456
51597
101921
85397
1.0
2.2
2.0
2.0
1.9
1.5
2.3
1.8
2.4
1.6
2.1
1.5
1.2
2.3
1.6
2.1
3.1
1.8
2.1
7.1
2.2
1.9
2.6
1.9
1.2
1.8
1.9
1.7
2.1
2.2
1.8
1.9
2.9
1.9
2.2
1.9
1.9
2.0
1.5
1.9
2.6
1.6
2.4
1.3
2.1
1.8
1.4
1.5
1.8
2.0
1.3
2.4
18.3288
18.1590
18.0169
17.9552
18.0312
18.0241
17.9575
17.8792
17.8740
17.7607
18.1547
17.5416
18.1200
17.4553
17.9144
17.9574
18.0630
18.0836
18.4005
17.9718
17.5484
17.6354
18.0512
17.8670
17.9413
18.4026
18.1773
18.2070
17.9748
18.0357
17.6772
18.1019
18.3276
18.1960
18.7253
17.8357
17.9398
17.9159
18.0941
18.0494
17.9743
17.9947
17.6622
18.1424
17.9521
17.8536
17.9165
17.9249
18.0399
18.3745
17.9813
17.6649
4.3
6.2
2.9
2.3
4.3
1.2
2.0
2.3
3.2
1.1
2.3
5.6
1.3
4.1
2.7
1.9
1.7
1.7
1.8
0.7
4.8
5.2
3.8
2.2
1.4
5.1
1.8
2.1
4.7
3.5
2.3
3.0
4.6
1.7
4.5
2.4
1.6
4.6
1.7
0.6
2.9
2.3
4.6
2.4
2.5
1.9
2.7
1.4
1.0
1.7
1.7
2.6
0.5025
0.5086
0.5127
0.5153
0.5136
0.5138
0.5159
0.5183
0.5186
0.5222
0.5113
0.5297
0.5134
0.5335
0.5201
0.5193
0.5163
0.5158
0.5071
0.5194
0.5319
0.5298
0.5178
0.5233
0.5211
0.5081
0.5145
0.5138
0.5209
0.5191
0.5301
0.5177
0.5120
0.5159
0.5017
0.5267
0.5239
0.5248
0.5204
0.5217
0.5239
0.5235
0.5334
0.5198
0.5254
0.5283
0.5265
0.5266
0.5232
0.5138
0.5250
0.5346
4.7
6.3
3.3
2.9
4.5
1.5
3.3
2.7
4.0
1.4
2.9
5.9
2.0
4.5
3.0
2.3
3.6
1.8
4.6
1.5
5.0
5.4
4.2
2.9
2.1
5.5
2.3
3.0
4.8
3.8
2.9
4.6
5.4
2.3
5.0
3.1
2.1
4.8
3.9
1.3
3.1
3.0
4.8
2.6
3.3
2.6
5.2
1.5
1.5
2.7
2.7
2.8
12MP07-54
12MP07-27
12MP07-66
12MP07-52
12MP07-34
12MP07-64
12MP07-63
12MP07-05
12MP07-50
12MP07-03
12MP07-99
12MP07-62
12MP07-61
12MP07-40
12MP07-48
12MP07-15
12MP07-70
12MP07-86
12MP07-16
12MP07-68
12MP07-75
12MP07-08
12MP07-55
190
96
87
264
212
181
282
140
121
786
53
159
252
279
237
129
260
194
187
208
66
247
65
53719
33811
35842
125039
89488
59639
138773
13549
99943
127309
16772
22935
148449
61904
82112
59298
73651
109849
50407
67859
3288
70661
31346
1.8
1.8
1.9
1.4
1.8
1.8
1.6
2.0
2.8
0.6
2.1
2.3
1.6
1.5
3.8
2.7
1.3
2.0
2.2
2.1
2.7
2.2
2.9
17.8950
18.0583
18.0986
17.9879
17.9712
17.8822
17.9250
17.9894
18.2591
17.9715
17.6231
18.1803
18.0237
17.9411
18.0865
17.6573
18.1104
18.2159
17.8006
18.2883
16.8360
17.9543
17.6527
3.3
3.5
3.8
1.2
1.9
2.1
1.5
4.1
3.4
0.8
6.2
3.6
1.7
1.3
2.4
4.4
1.9
2.6
2.4
1.7
9.7
1.2
3.2
0.5296
0.5248
0.5243
0.5277
0.5283
0.5311
0.5300
0.5283
0.5206
0.5290
0.5396
0.5232
0.5288
0.5317
0.5275
0.5429
0.5296
0.5274
0.5403
0.5330
0.5805
0.5486
0.5668
4.6
4.7
4.4
2.0
2.9
3.0
2.0
4.3
3.7
1.2
6.5
3.8
3.5
5.8
3.2
4.8
2.0
4.5
3.1
3.1
11.0
9.4
4.1
12MP08; Yukon-Tanana, Endicott Arm Assemblage, meta-rhyolite, (Degree Decimal: 55.44693, 13
12MP08-21R
348
303965
1.8 18.3058
1.6
0.4627
2.7
12MP08-18C
208
59476
2.2 17.8347
2.1
0.4839
2.9
12MP08-5R
244
271408
2.6 18.3338
2.2
0.4708
3.1
12MP08-5C
168
52466
3.2 18.5070
3.4
0.4697
4.2
12MP08-14R
158
20953
3.2 17.9307
2.6
0.4861
2.8
12MP08-6C
96
44438
3.2 18.4453
6.4
0.4740
6.9
12MP08-4R
325
93453
2.1 18.1116
1.5
0.4835
2.2
12MP08-4C
223
110365
2.6 18.1167
1.9
0.4834
3.5
12MP08-16R
174
60826
2.9 18.3697
3.6
0.4780
3.8
12MP08-6R
261
110373
3.2 18.4734
1.5
0.4756
2.4
12MP08-2C
136
27884
3.1 18.5253
5.0
0.4744
7.8
12MP08-19R
351
133662
2.5 18.2530
1.5
0.4820
3.3
12MP08-9R
279
160104
2.8 18.0757
2.3
0.4884
3.1
12MP08-7R
178
60677
3.4 18.4570
4.7
0.4784
5.5
12MP08-2R
210
101994
3.3 18.3948
3.1
0.4811
3.5
12MP08-3C
266
105491
2.6 18.1473
1.3
0.4881
4.2
12MP08-17R
418
160147
1.8 18.1435
0.8
0.4889
2.4
12MP08-8R
178
102837
2.8 18.3490
2.1
0.4848
4.3
12MP08-12R
245
94511
3.3 18.1153
1.8
0.4912
2.2
12MP08-11R
276
133358
2.3 17.9926
1.9
0.4947
2.7
12MP08-1C
147
41203
3.5 18.4239
3.6
0.4839
5.0
12MP08-13R
156
51229
3.6 18.2878
2.4
0.4877
3.0
12MP08-15R
144
61058
3.2 17.9820
2.7
0.4976
3.0
12MP08-3R
262
103773
2.4 18.4455
2.0
0.4861
2.5
12MP08-10R
218
69710
2.3 18.1274
1.9
0.5048
2.7
12MP08-22R
174
3810
2.3 17.5530
2.3
0.5274
3.8
12MP08-1R
234
121042
2.9 18.2769
2.2
0.5105
2.7
12MP09; Yukon-Tanana, meta-trondjemite, (Degree Decimal: 55.44693, 131.32267)
811
38157
1.2 18.1850
1.1
0.4106
12MP09-9
12MP09-17
81
40095
4.3 18.9168
4.6
0.4688
12MP09-4
123
66443
3.2 18.5123
2.7
0.5022
12MP09-1R
213
63038
2.6 17.6780
3.1
0.5324
12MP09-18
204
45658
2.6 17.5649
3.0
0.5359
12MP09-15
213
119868
2.0 18.3396
3.0
0.5143
12MP09-10
92
31315
3.2 17.9602
8.5
0.5266
12MP09-6
156
68943
2.7 18.1116
3.0
0.5228
12MP09-14
153
185584
2.1 18.4042
3.0
0.5156
12MP09-8
153
38529
2.8 17.5540
4.4
0.5408
12MP09-23
146
130143
2.8 17.6896
3.8
0.5373
12MP09-12
139
43461
2.5 18.2759
3.4
0.5215
12MP09-16
184
55970
2.2 18.3033
1.6
0.5218
12MP09-13
123
38228
3.1 18.2974
9.2
0.5221
12MP09-1C
155
60014
2.1 18.0816
4.1
0.5283
12MP09-3C
127
33772
2.9 18.0888
6.4
0.5288
12MP09-2C
122
52387
2.5 17.7321
4.3
0.5397
12MP09-19
147
97799
2.8 18.3261
4.0
0.5222
12MP09-11
133
39662
2.8 18.1922
4.0
0.5290
12MP09-5
159
48114
3.0 18.4159
2.9
0.5227
12MP09-20
172
118940
1.6 17.9735
3.6
0.5360
12MP09-3R
118
36499
2.7 18.2976
3.6
0.5272
12MP09-24
45
16172
3.6 16.8680
15.1
0.5726
12MP09-7
151
83785
2.7 18.3956
3.1
0.5251
12MP09-22
215
69209
2.2 18.2426
2.8
0.5323
12MP09-21
69
38668
2.8 17.5552
4.7
0.5670
12MP09-2R
65
20181
3.4 18.1465
10.1
0.5655
2.6
5.5
3.7
3.4
3.2
3.2
8.7
3.2
3.3
4.8
4.4
3.7
2.2
9.2
5.0
6.5
4.9
4.2
4.2
3.5
4.2
4.0
15.6
3.4
4.6
5.1
11.7
12MP10; Yukon-Tanana, Tracy Arm Assemblage, ortho-quartzite with marble layers, (Degree Deci
12MP10-1
291
58694
2.7 19.3896
0.7
0.2506
1.9
187
133747
2.0 19.4442
1.3
0.2680
1.5
12MP10-3
271
21632
0.9 16.6765
11.4
0.3445
12.1
12MP10-4
966
396979
12.0 19.0813
0.9
0.3191
1.7
12MP10-5
304
123325
1.6 19.2083
1.0
0.2758
1.8
12MP10-6
12MP11; Yukon-Tanana, Tracy Arm Assemblage, ortho-quartzite with marble layers, (Degree Deci
12MP11-15
465
18297
1.9 22.6337
9.3
0.0922
9.3
12MP11-01
114
7548
4.2 20.8865
18.1
0.1425
19.3
12MP11-02
380
26887
3.5 19.3178
5.3
0.1762
6.1
12MP11-32
923
35397
0.6 19.1276
1.4
0.2700
2.6
12MP11-03
428
61160
1.8 19.4287
1.7
0.2700
2.5
12MP11-46
712
114565
1.9 19.3715
1.4
0.2731
2.2
12MP11-24
839
117572
0.9 19.5761
1.8
0.2724
1.9
12MP11-21
522
19398
1.1 19.1072
2.7
0.2870
3.1
12MP11-47
554
52015
0.8 19.1209
2.5
0.2870
4.7
12MP11-43
348
6259
1.7 18.7243
4.9
0.2933
5.0
12MP11-17
339
46395
1.7 19.7715
2.4
0.2782
3.6
12MP11-42
345
47835
1.7 19.2707
2.9
0.2864
3.0
12MP11-05
144
16879
2.0 20.1698
11.9
0.2751
12.9
12MP11-27
709
47239
0.9 19.0342
2.0
0.2953
3.1
12MP11-07
12MP11-35
12MP11-18
12MP11-14
12MP11-23
12MP11-29
12MP11-44
12MP11-39
12MP11-38
12MP11-06
12MP11-30
12MP11-40
12MP11-36
12MP11-28
12MP11-45
12MP11-22
12MP11-04
12MP11-37
12MP11-31
12MP11-08
12MP11-41
12MP11-26
12MP11-10
12MP11-20
12MP11-09
12MP11-12
12MP11-19
12MP11-13
12MP11-33
569
414
349
335
503
264
445
429
560
290
345
514
379
323
672
107
203
78
122
149
222
259
963
198
274
162
152
136
36
116802
65282
30639
62994
95609
41096
31250
43441
42864
8024
51442
16854
35963
48643
7685
12781
2448
10925
6477
43885
55561
32274
32586
40763
129131
25205
17106
35615
23110
1.1
1.8
1.5
2.0
1.2
1.5
1.3
1.7
2.0
1.5
1.6
1.9
1.7
2.0
1.4
1.3
0.7
2.0
1.2
2.1
0.9
0.6
2.6
0.8
2.7
2.5
1.1
1.5
2.3
19.1959
19.7716
19.4739
19.7827
19.6384
19.2293
19.2211
19.2389
19.5388
19.0458
19.2283
19.1559
19.3894
19.1317
18.8123
19.3165
18.5937
20.9075
18.7026
19.5039
19.2306
19.0691
18.2723
19.9872
19.1862
19.4159
17.5627
17.7974
9.6746
0.8
2.2
2.3
2.6
1.8
3.9
2.7
2.3
1.6
5.0
3.0
2.2
2.3
3.3
3.0
10.2
3.4
12.4
8.6
8.0
3.4
3.7
0.8
6.7
3.1
5.4
6.2
5.4
2.8
0.2936
0.2855
0.2901
0.2859
0.2880
0.2944
0.2946
0.2946
0.2920
0.2997
0.2970
0.2981
0.2981
0.3024
0.3081
0.3004
0.3134
0.2787
0.3116
0.3007
0.3222
0.3325
0.3507
0.3278
0.4021
0.4053
0.5205
0.5387
3.7073
2.8
2.8
3.0
2.9
2.2
4.6
4.7
2.7
1.7
5.2
3.0
2.3
2.6
7.3
3.9
10.4
3.7
13.0
9.6
8.1
3.6
4.0
2.6
6.8
3.3
7.5
7.2
5.7
6.4
12MP12; Yukon-Tanana, Tracy Arm Assemblage, quartzite layers with marble, (Degree Decimal: 5
12MP12-87
320
18155
6.1 20.5574
1.8
0.0576
2.5
12MP12-19
275
28419
28.4 19.6133
1.8
0.1571
3.5
12MP12-29
1158
110982
12.5 10.6135
1.6
0.4067
1.9
174
34335
2.8 18.2470
0.8
0.4040
1.0
12MP12-64
12MP12-98
674
139240
3.7 18.3207
1.0
0.4100
2.1
12MP12-122
833
372736
1.9 18.0748
1.1
0.4494
1.3
12MP12-120
377
263208
3.7 18.0342
0.8
0.4788
3.5
12MP12-101
221
380786
1.3 18.0653
0.6
0.4886
1.0
12MP12-04
548
525008
1.5 17.9843
1.1
0.5019
3.6
12MP12-05
319
106118
1.9 17.9616
0.7
0.5078
1.8
12MP12-38
283
132366
0.9 17.3600
0.9
0.5345
2.1
12MP12-03
179
102825
5.3 16.3727
0.6
0.8728
1.3
12MP12-55
187
128873
1.7 15.3743
1.3
1.0827
2.8
12MP12-106
150
383083
2.5 13.8568
0.9
1.3026
2.1
12MP12-12
190
295060
1.2 14.1731
0.9
1.2915
4.5
12MP12-112
151
90808
2.0 14.1988
0.7
1.3840
1.6
12MP12-49
678
606890
19.3 13.9063
2.0
1.4571
3.6
12MP12-90
278
218015
3.5 13.8753
0.8
1.4616
1.9
12MP12-24
269
223209
1.3 13.6049
0.7
1.6109
1.6
12MP12-46
583 1547446
4.5 13.4400
1.5
1.5216
3.2
12MP12-123
201
221150
1.5 13.3109
0.8
1.7586
3.0
12MP12-67
12MP12-76
12MP12-104
12MP12-48
12MP12-84
12MP12-116
12MP12-16
12MP12-54
12MP12-43
12MP12-11
12MP12-97
12MP12-81
12MP12-88
12MP12-62
12MP12-61
12MP12-103
12MP12-94
12MP12-86
12MP12-37
12MP12-100
12MP12-14
12MP12-75
12MP12-78
12MP12-109
12MP12-79
12MP12-69
12MP12-59
12MP12-82
12MP12-47
12MP12-107
12MP12-22
12MP12-21
12MP12-06
12MP12-71
12MP12-68
12MP12-117
12MP12-30
12MP12-58
12MP12-91
12MP12-45
12MP12-18
12MP12-10
12MP12-115
12MP12-99
12MP12-42
12MP12-23
12MP12-108
12MP12-60
12MP12-28
12MP12-51
12MP12-114
12MP12-53
188
98
73
174
42
590
203
131
56
273
113
111
33
161
443
255
788
78
287
65
141
87
53
82
230
146
60
87
164
237
30
89
42
127
35
261
79
160
109
99
568
38
391
119
38
159
167
66
181
45
76
25
175925
583498
119316
120412
42274
617124
223205
165570
70179
452457
201437
234803
48616
325209
777386
572516
410353
71947
337524
58473
116190
261768
163188
89595
216440
465513
134577
225647
144306
351314
68431
244706
165079
188396
159576
287230
123094
92473
193619
154705
817875
58814
574872
288788
114641
515054
158436
197439
639161
216584
202589
41282
0.6
2.1
3.2
1.5
1.6
2.0
1.6
1.1
1.8
1.7
2.0
1.9
2.3
1.1
2.1
98.4
1.6
3.6
2.5
2.2
1.5
2.1
1.6
2.8
70.1
2.2
1.3
1.2
1.9
2.7
1.3
1.0
0.8
2.0
1.1
1.7
2.1
1.7
1.0
1.2
1.0
10.0
3.7
1.3
2.2
2.1
2.4
1.4
1.2
2.7
1.4
0.7
13.3017
13.2642
13.2592
13.2405
13.2028
13.1634
13.1389
13.1309
13.0523
12.8668
12.8471
12.7560
12.7366
12.5999
12.5925
12.5237
12.4948
12.1114
11.9587
11.7166
11.5881
11.4849
11.4699
11.3408
11.0847
11.0437
10.9402
10.8365
10.6554
10.4172
10.1231
10.0691
9.9861
9.9737
9.9689
9.9480
9.9161
9.8445
9.8366
9.7780
9.5135
9.4625
9.3897
9.3762
9.3225
8.8343
8.7526
8.6767
8.4772
8.2830
8.0224
7.7878
0.9
0.6
0.8
1.6
1.2
1.7
0.8
0.7
0.8
1.0
1.1
0.6
1.6
0.5
0.6
0.8
1.3
0.9
0.9
0.8
0.8
0.6
1.1
4.7
1.3
0.9
0.9
0.7
0.8
3.6
0.9
0.9
0.8
0.9
0.7
1.1
0.6
1.1
0.9
0.6
2.0
0.8
1.5
0.5
1.0
0.8
0.6
0.6
1.1
0.9
0.7
1.0
1.7263
1.8279
1.7020
1.5155
1.5308
1.8960
1.8781
1.6519
1.7665
1.7750
2.0922
2.0914
1.7763
2.0988
2.0083
1.9764
1.8388
2.0379
2.4093
2.6706
2.5090
2.5335
2.5949
2.3357
2.7446
2.8214
2.9638
2.7420
3.0575
3.2035
3.2299
3.1885
3.7579
3.9653
3.5179
3.4010
3.1987
3.3806
3.6525
3.6310
4.0912
4.1249
3.8593
4.3259
4.5038
4.7578
4.1262
4.6762
4.7197
5.3377
5.9072
6.3181
5.1
1.9
5.4
2.4
4.0
2.5
2.1
2.2
2.3
1.7
1.9
1.6
2.2
1.0
4.7
3.8
3.9
2.6
1.3
2.9
2.6
1.7
1.8
5.8
2.7
2.0
1.2
1.9
2.0
4.4
1.4
2.4
2.3
1.7
1.6
2.7
3.9
1.3
1.5
1.3
3.1
1.7
3.2
1.3
2.1
2.4
3.1
1.2
1.5
4.2
3.0
2.5
12MP12-20
12MP12-17
12MP12-44
12MP12-113
12MP12-25
49
236
181
294
93
114838
578287
661069
780875
177697
0.7
2.5
6.8
1.7
1.1
5.3955
5.3803
5.2993
5.0008
4.9615
0.8
1.4
1.7
1.4
0.7
12.0863
10.4043
11.4884
13.0849
11.8828
3.8
4.0
2.7
1.8
2.0
12MP13; Yukon-Tanana, quartzite, (Degree Decimal: 56.21072, 131.56384)
12MP13-70
450
15855
4.8 20.6826
6.8
12MP13-24
2710
72715
27.8 20.6953
1.0
12MP13-104
342
15856
38.2 21.9991
17.2
12MP13-72
346
19234
45.8 19.6560
10.2
12MP13-91
796
61555
10.4 19.2289
1.6
321
88200
5.1 14.7734
1.9
12MP13-58
12MP13-109
197
38423
8.0 19.0511
3.2
12MP13-88
116
55462
2.0 18.8564
5.6
12MP13-31
136
42393
9.0
8.0258
4.3
12MP13-25
1884
64140
5.6 18.0720
0.6
12MP13-64
3170
109321
30.2 18.2233
0.3
12MP13-85
1153
54829
2.0 17.9205
0.8
12MP13-55
115
17072
2.5 18.1401
4.2
12MP13-49
214
55701
1.3 18.2119
2.4
12MP13-27
1038
189048
1.7 17.9885
0.3
12MP13-76
513
243386
1.6 17.8786
1.1
12MP13-82
1184
244912
1.0 17.9192
0.4
12MP13-71
128
28430
1.0 18.0634
4.3
12MP13-102
976
569876
2.7 17.9985
0.7
12MP13-10
147
62450
1.0 18.4719
2.7
12MP13-108
28
9242
1.6 18.7805
13.6
173
59828
3.0 13.2182
2.0
12MP13-29
12MP13-25
501
203089
4.5 17.0132
0.6
12MP13-105
118
78328
0.9 16.0300
2.3
12MP13-103
190
227285
4.9 14.3225
1.2
12MP13-11
126
66793
3.3 14.1107
1.9
12MP13-93
50
53298
1.7 13.7016
3.1
12MP13-106
156
110558
2.8 13.5986
1.0
12MP13-69
200
145626
1.8 13.5912
0.7
12MP13-60
20
14002
1.4 13.5570
6.1
12MP13-36
59
51253
1.5 13.2874
1.8
12MP13-81
1521
886652
3.7 13.1110
0.2
12MP13-14
74
7939
1.3 12.9551
3.1
12MP13-46
162
91199
2.4 12.9077
1.1
12MP13-01
79
43238
1.3 12.8671
1.7
12MP13-63
73
78521
2.4 12.8635
2.1
12MP13-56
69
112469
1.2 12.8295
2.0
12MP13-57
24
30020
0.9 12.8209
5.6
12MP13-99
42
67659
1.4 12.7175
3.3
12MP13-74
246
151609
3.2 12.6738
0.4
12MP13-08
155
152043
2.0 12.3045
1.0
12MP13-110
100
66010
4.5 11.9706
1.6
12MP13-96
85
16750
1.8 11.8524
6.1
12MP13-02
356
291858
1.9 11.7688
0.4
12MP13-53
86
85524
0.9 11.7052
1.2
0.0587
0.0588
0.0590
0.0667
0.2133
0.3860
0.3076
0.3146
0.7907
0.4109
0.4416
0.4546
0.4776
0.4781
0.4989
0.5131
0.5168
0.5186
0.5216
0.5196
0.5581
0.9126
0.7445
0.9270
1.4457
1.5471
1.6262
1.6253
1.6814
1.7662
1.8687
1.7414
1.8811
1.9027
1.9930
2.0398
1.9927
2.0477
1.9393
2.0460
1.9650
2.0975
2.2343
2.3450
2.3096
7.0
1.4
17.4
10.7
3.6
9.1
5.0
8.2
6.5
1.6
1.9
3.5
7.4
3.2
6.2
2.0
1.1
6.4
3.5
3.8
14.3
7.0
2.1
9.7
2.5
3.4
3.6
3.5
1.2
8.2
4.1
2.9
3.6
4.5
5.2
4.5
3.8
9.1
3.7
1.3
5.0
4.6
9.0
2.2
4.6
12MP13-20
12MP13-68
12MP13-40
12MP13-90
12MP13-59
12MP13-22
12MP13-98
12MP13-101
12MP13-77
12MP13-19
12MP13-35
12MP13-07
12MP13-09
12MP13-65
12MP13-84
12MP13-33
12MP13-100
12MP13-80
12MP13-83
12MP13-89
12MP13-94
12MP13-44
12MP13-28
12MP13-47
12MP13-23
12MP13-51
12MP13-04
12MP13-41
12MP13-50
12MP13-03
12MP13-05
12MP13-30
12MP13-45
12MP13-92
54
95
358
31
177
483
261
158
204
150
191
82
569
61
125
773
102
495
72
64
204
155
168
214
91
111
385
138
215
100
39
31
187
49
58250
150101
50221
32942
146286
169864
219595
122085
43215
203253
168007
155171
361580
27621
148722
687533
148706
135718
86740
76964
256876
84289
319367
183179
122507
206378
303386
300119
791023
207625
112051
59577
141776
128039
1.2
2.2
3.5
1.2
2.2
2.0
2.7
2.6
8.3
2.6
1.1
1.6
1.6
1.6
1.8
3.0
0.7
0.6
0.6
1.2
0.7
3.7
0.8
3.5
2.6
1.5
2.5
0.7
1.1
0.9
0.9
0.7
1.3
0.7
11.6666
11.4089
11.3219
11.1490
11.0157
10.9608
10.9381
10.9284
10.7743
10.7727
10.7390
10.7190
10.7003
10.6923
10.6728
10.6646
10.0552
10.0488
9.9944
9.8784
9.8700
9.8674
9.7430
9.5667
9.3932
9.3683
9.2276
9.1271
9.0573
8.1134
5.9563
5.5044
5.3377
4.5845
2.2
0.9
0.9
3.7
0.4
0.9
0.5
0.4
1.4
0.6
0.8
0.8
0.2
1.7
0.7
0.2
0.9
0.3
1.0
1.5
0.3
0.5
0.4
0.4
0.7
0.8
0.4
0.4
0.3
0.6
0.8
0.8
0.2
0.4
2.6377
2.7572
1.1120
2.7091
2.8798
3.0950
2.9419
3.1595
1.2345
3.0497
2.9822
3.1896
3.0968
3.0313
3.0507
3.3344
3.5221
3.0814
3.9370
3.3381
3.7095
3.3492
3.8234
3.4855
4.1848
4.4144
4.3981
4.7339
4.5517
4.8416
9.0674
12.6298
11.3151
16.4466
12MP14; Yukon-Tanana, quartzite layers with marble, (Degree Decimal: 56.18398, 131.65540)
12MP14-32
613
16520
120.7 20.7555
0.7
0.0701
12MP14-26
267
3269
96.5 21.0637
0.9
0.0737
12MP14-22
258
6841
138.8 20.6439
1.0
0.0814
12MP14-30
227
6299
56.3 20.4404
1.8
0.0861
12MP14-09
2771
35757
22.7 20.4649
0.9
0.0879
12MP14-35
141
2386
93.3 21.4747
2.5
0.0838
12MP14-12
254
13374
56.7 20.1598
1.4
0.0896
12MP14-31
129
2751
26.6 19.7151
1.9
0.0920
12MP14-17
809
23611
124.6 20.6886
1.4
0.0925
12MP14-34
55
2279
126.4 20.1112
3.3
0.0962
12MP14-13
6154
58095
9.9 20.8696
0.8
0.0956
12MP14-01
39
2267
80.7 18.5249
4.0
0.1086
12MP14-24
3277
66510
52.5 20.6369
1.1
0.0996
12MP14-10
3133
57286
14.7 20.0025
2.3
0.1040
12MP14-11
3101
45514
10.8 20.5540
0.7
0.1024
12MP14-16
200
3662
89.2 21.0329
1.4
0.1047
3.3
2.4
5.7
5.5
3.1
3.8
3.2
1.6
6.0
2.3
2.0
3.3
2.4
4.6
4.8
1.7
4.2
1.5
2.7
7.7
3.8
4.7
4.9
6.1
3.7
2.2
1.9
1.2
2.2
2.1
3.6
3.7
2.6
2.1
2.2
1.3
3.3
2.4
2.0
4.9
3.0
3.0
7.6
5.2
1.5
5.4
1.6
2.5
2.0
4.4
12MP14-28
12MP14-33
12MP14-06
12MP14-25
12MP14-14
12MP14-02
12MP14-18
12MP14-05
12MP14-21
12MP14-07
12MP14-04
12MP14-27
12MP14-23
12MP14-08
12MP14-19
2817
774
1604
965
125
303
1006
569
309
241
204
417
235
460
150
11932
11619
89531
65383
16086
24290
47651
45123
32119
10961
8586
215518
24394
89087
7652
4.4
72.7
0.9
3.0
1.4
2.7
0.9
1.0
1.3
1.6
15.0
1.8
27.7
1.1
2.0
19.8549
20.3650
19.9464
20.1286
19.2110
18.7478
19.9342
19.7818
19.7991
19.7343
19.8499
19.7220
19.8002
19.5713
20.1767
0.7
3.7
0.7
0.7
2.4
0.6
0.6
0.7
0.8
0.6
1.2
0.6
0.6
0.7
0.8
0.1126
0.1160
0.1297
0.1286
0.1806
0.2069
0.1967
0.2092
0.2184
0.2206
0.2214
0.2272
0.2269
0.2336
0.2272
3.3
4.8
6.4
2.1
7.5
6.9
1.2
1.7
2.0
2.5
4.5
3.9
1.4
1.3
3.0
12MP15; Yukon-Tanana, tonalite orthogneiss, (Degree Decimal: 56.21648, 131.80635)
12MP15-3
617
52033
1.5 19.8691
1.8
0.0903
12MP15-7C
425
24367
3.8 20.6902
0.8
0.0897
12MP15-7R
291
27005
7.1 20.7503
0.6
0.0903
12MP15-3C
263
25253
5.1 20.5952
2.3
0.0926
12MP15-4R
287
49968
5.0 21.2009
0.7
0.0903
12MP15-5
129
24940
8.9 21.2112
3.8
0.0906
12MP15-3R
431
30892
5.6 20.7698
1.1
0.0930
12MP15-7RR
304
21656
8.7 21.0200
1.2
0.0930
12MP15-7
210
23876
6.0 20.9596
1.3
0.0937
12MP15-1C
480
61551
3.4 20.3252
2.2
0.0968
12MP15-3RR
420
50383
4.7 21.6657
0.5
0.0936
12MP15-1R
994
65708
6.7 20.8876
0.5
0.0975
12MP15-5R
1004
120094
19.0 20.6542
0.6
0.0990
12MP15-1RR
373
33797
3.9 22.2132
1.7
0.0925
12MP15-6R
382
10126
6.5 18.3772
9.9
0.1124
12MP15-4R
183
19640
3.6 21.2994
0.9
0.1039
12MP15-5R
269
24537
11.2 21.8190
1.5
0.1093
12MP15-4C
357
36164
1.6 20.5205
0.6
0.1489
2516
166018
5.5 18.8236
0.7
0.1849
12MP15-4
12MP15-5C
500
70604
1.8 20.0065
0.6
0.1749
12MP15-6C
624
84459
1.6 20.0838
0.9
0.1866
12MP15-6
224
39690
1.2 20.0310
0.9
0.1907
12MP15-6RR
283
47027
2.5 20.0333
1.1
0.1907
12MP15-2
203
34627
1.6 19.9068
1.0
0.1946
12MP15-1
472
97403
1.7 20.1330
0.9
0.1963
12MP15-2R
222
89007
2.8 19.7047
1.0
0.2166
12MP15-2C
117
31224
1.7 19.3077
0.9
0.3898
3.9
1.2
3.1
3.4
2.3
3.9
2.5
2.9
1.8
2.9
1.1
3.0
2.6
1.8
10.6
3.3
5.2
2.3
4.8
1.7
1.3
2.0
1.8
1.5
2.9
5.7
2.0
12MP16; Yukon-Tanana, Endicott Arm Assemblage, quartzite with marble (Degree Decimal: 56.21
12MP16-13
961
16694
42.2 21.9117
4.6
0.0677
4.7
12MP16-08
69
2546
217.1 21.3689
45.7
0.0842
46.1
12MP16-48
126
5769
278.4 19.6652
33.5
0.0915
33.6
12MP16-41
70
3529
15.9 23.6684
38.8
0.0765
39.4
12MP16-52
543
13547 27055.7 22.3061
5.6
0.0818
5.7
12MP16-55
640
35102
187.1 23.3140
3.9
0.0784
4.3
12MP16-16
12MP16-33
12MP16-28
12MP16-04
12MP16-14
12MP16-06
12MP16-35
12MP16-50
12MP16-51
12MP16-03
12MP16-49
12MP16-56
12MP16-17
12MP16-15
12MP16-36
12MP16-09
12MP16-21
12MP16-64
12MP16-63
12MP16-11
12MP16-19
12MP16-23
12MP16-53
12MP16-12
12MP16-37
12MP16-26
12MP16-27
12MP16-61
12MP16-46
12MP16-40
12MP16-47
12MP16-34
12MP16-62
12MP16-45
12MP16-58
12MP16-39
12MP16-05
12MP16-02
12MP16-29
12MP16-57
12MP16-31
12MP16-65
12MP16-18
12MP16-38
12MP16-22
12MP16-54
12MP16-25
12MP16-10
12MP16-42
904
667
606
399
1147
231
480
374
1389
613
492
609
1106
276
285
1689
290
132
1485
2162
979
3165
2731
853
1496
111
104
494
1017
316
2957
101
1682
479
640
2044
466
2034
85
106
460
98
486
526
108
219
3455
217
2621
51932
62403
23066
18073
51823
66443
25791
24695
57091
40053
29599
21014
58407
16118
14337
94933
16384
5806
109291
74737
33304
875099
28696
46078
57551
4076
3987
28073
49536
27948
180339
7216
154326
26225
41491
81617
30382
96637
3223
5412
56553
5195
29880
89770
7414
4751
235057
1844
16795
39.8
124.0
596.4
284.6
753.4
2589.1
70017.5
1583.0
110.6
4037.4
264.1
3069.1
250.1
1571.2
327.7
1145.6
19263.9
11.7
592.5
238.1
240.4
68.1
527.5
175.9
209.5
8.1
94.0
242.2
568.6
172.9
194.4
21.2
213.9
97.5
61.5
563.4
36.8
88.6
15.3
11.5
100.8
317.3
25.3
53.8
11.5
43.9
95.3
6.7
8.7
21.1541
20.7945
22.6091
22.5603
20.9293
20.3143
21.8068
20.5361
21.1370
21.0141
20.6203
20.3331
20.2742
23.6786
19.4068
20.8729
19.9631
26.1566
20.8076
20.8349
20.7524
20.7691
20.5044
20.5517
21.1689
21.4343
23.5709
21.4207
20.7987
22.0826
20.6093
22.1591
20.8168
21.2579
21.1486
20.6065
20.0246
20.8836
5.6656
19.4603
20.4904
29.7953
20.7195
20.6496
22.0715
18.2701
20.8087
21.8308
20.4843
2.1
4.8
5.5
10.2
2.9
16.3
9.3
14.3
4.9
5.6
7.7
5.7
3.0
13.4
11.8
2.5
10.6
27.6
2.8
1.8
3.1
1.0
4.0
4.3
2.9
26.5
45.8
5.2
3.3
11.9
1.3
20.0
2.6
4.9
4.8
1.7
5.8
1.7
443.2
24.8
6.5
33.8
5.3
5.4
28.3
17.0
0.9
15.8
1.9
0.0864
0.0884
0.0813
0.0815
0.0879
0.0908
0.0848
0.0901
0.0878
0.0883
0.0900
0.0914
0.0917
0.0786
0.0960
0.0893
0.0935
0.0714
0.0902
0.0901
0.0905
0.0905
0.0918
0.0917
0.0891
0.0882
0.0803
0.0883
0.0912
0.0860
0.0925
0.0862
0.0918
0.0902
0.0908
0.0933
0.0962
0.0923
0.3406
0.0992
0.0942
0.0651
0.0938
0.0941
0.0885
0.1073
0.0944
0.0951
0.1020
2.6
5.4
5.7
10.4
3.1
16.6
9.7
14.4
4.9
5.9
7.9
5.8
3.2
13.5
12.1
2.8
10.8
28.2
3.0
1.8
3.3
1.4
4.4
4.5
3.0
26.9
46.2
5.5
3.5
12.0
1.6
21.5
2.8
5.5
5.4
1.9
6.0
1.8
443.2
25.4
6.7
34.2
5.7
5.5
28.6
18.0
1.3
16.3
2.6
12MP17; Yukon-Tanan, Endicott Arm Assemblage, clean quatzite in marble sequence, (Degree De
12MP17-01
124
1604
0.9 15.7828
9.9
0.8308
10.6
12MP17-03
12MP17-04
57
73
41713
14638
1.4
1.0
12.1919
9.8027
1.9
1.4
2.4712
3.8399
2.6
5.3
12MP18; Yukon-Tanana, Endicott Arm Assemblage, meta-conglomerate, (Degree Decimal: 56.362
12MP18-2
111
9896
1.7 20.4512
2.3
0.0792
2.6
12MP18-4
81
23798
0.7 18.4376
1.3
0.4287
2.0
12MP18-5
185
171154
1.5 18.6298
0.8
0.4029
2.0
12MP19; Yukon-Tanana, Endicott Arm Assemblage, meta-rhyolite, (Degree Decimal: 56.37230, 132
12MP19-6C
384
49641
3.0 18.9003
3.4
0.3003
5.3
12MP19-7
110
4037
1.9 17.6717
9.6
0.4058
10.3
12MP19-4C
84
16471
2.6 19.2151
6.5
0.4152
6.8
12MP19-11C
100
12618
2.1 18.3319
6.0
0.4467
6.3
12MP19-3R
62
23117
2.6 17.0390
7.7
0.4842
8.4
12MP19-9
121
8885
1.9 17.8509
4.4
0.4627
4.6
12MP19-2C
127
2680
2.0 17.3655
7.8
0.4766
7.9
12MP19-5
80
19555
2.3 18.5509
6.4
0.4508
6.5
12MP19-13
153
36580
2.4 18.0296
5.0
0.4686
5.4
12MP19-12
208
33722
2.0 18.3737
3.4
0.4600
4.1
12MP19-6R
72
26630
2.8 18.1885
4.4
0.4652
5.3
12MP19-1
100
32936
1.9 17.8099
6.1
0.4793
6.4
12MP19-8
98
21910
2.3 19.0473
7.9
0.4531
9.0
12MP19-10C
86
3443
1.9 16.1649
17.7
0.5401
18.2
12MP20; Yukon-Tanana, Endicott Arm Assemblage, meta-rhyolite, (Degree Decimal: 57.02759, 132
12MP20-05R1
527
17336
58.1
8.3567
2.6
0.1469
4.3
12MP20-05R2
546
25657
56.1
8.1707
4.2
0.1581
4.7
12MP20-14R1
1454
160279
1043.8 20.7154
0.6
0.0819
1.0
12MP20-17R1
1020
73264
1546.6 20.6660
0.7
0.0832
3.3
12MP20-22R2
891
358013
1006.6 20.8195
1.2
0.0842
2.7
12MP20-02
1126
118229
807.8 20.5567
0.9
0.0860
2.0
12MP20-16R1
1316
91082
929.9 20.6114
0.7
0.0861
1.7
12MP20-04
1149
129949
21.3 20.0540
1.1
0.0898
9.1
12MP20-05M
806
64549
499.8 19.4320
3.2
0.0942
5.0
12MP20-31
4780
259329
78.8 20.4423
1.1
0.0925
1.5
12MP20-22R
1431
73691
1040.5 20.4898
2.4
0.0950
2.4
12MP20-38
1286
33117
73.1 20.1678
0.7
0.0989
2.5
12MP20-46
2259
16622
10.2 17.2282
4.3
0.1272
10.6
12MP20-13
3595
183828
3.5 19.9368
0.8
0.1128
3.1
12MP20-43
3175
61012
0.5 19.4284
1.0
0.1278
2.4
12MP20-21
1049
240055
1.4 18.6003
0.9
0.2745
2.5
12MP20-41
369
118091
1.6 18.5217
1.1
0.2937
6.2
12MP20-32
365
77339
2.6 18.6246
1.1
0.3097
4.7
12MP20-36
819
287133
2.0 18.6703
0.8
0.3287
5.8
12MP20-9
1307
250782
0.9 18.3754
0.8
0.3564
1.6
12MP20-7
402
189844
1.5 18.2760
0.8
0.3710
2.4
12MP20-44
383
90865
1.2 18.6182
0.8
0.3910
1.5
12MP20-10
739
584522
0.8 18.2888
0.5
0.4173
1.6
12MP20-29
385
174739
1.2 18.3943
0.8
0.4235
1.1
12MP20-28
695
296832
0.7 18.2881
0.8
0.4292
1.0
12MP20-05
341
84743
1.2 18.1584
0.7
0.4327
2.2
12MP20-30
279
497817
2.0 18.6083
1.2
0.4223
3.4
12MP20-11
12MP20-34
12MP20-26
12MP20-12
12MP20-42
12MP20-24
12MP20-25
12MP20-22
12MP20-15
12MP20-17
12MP20-33
12MP20-01
12MP20-35
12MP20-14
12MP20-22M
12MP20-18
12MP20-27
12MP20-16
12MP20-20
258
421
499
580
139
390
249
122
492
321
397
238
307
252
265
406
399
252
1046
92153
95803
93005
158134
113193
190110
96083
34188
206869
130382
158065
129888
136837
61355
135284
110453
195662
67761
328821
1.2
1.6
1.3
3.1
1.5
0.6
1.9
1.7
0.7
1.4
1.3
1.3
1.6
1.9
1.2
1.6
1.2
1.4
1.1
18.1524
18.4816
18.2257
18.6228
18.1696
18.3788
18.4603
18.3475
18.4947
18.3966
18.4512
18.3069
18.4960
18.5765
18.3808
18.4035
18.1164
18.4302
17.9741
1.4
1.0
1.0
1.6
1.9
0.6
0.7
0.9
0.9
1.1
0.6
0.9
0.9
0.9
0.8
0.9
0.8
0.9
0.6
0.4372
0.4305
0.4369
0.4286
0.4422
0.4382
0.4371
0.4414
0.4386
0.4422
0.4423
0.4462
0.4433
0.4422
0.4516
0.4524
0.4599
0.4543
0.4870
1.5
2.1
1.9
3.0
2.1
1.4
1.5
1.5
2.0
1.8
1.5
2.2
1.2
1.7
1.9
2.6
3.1
1.1
0.9
12MP23; Yukon-Tanana, Endicott Arm Assemblage, quartzite, (Degree Decimal: 57.33710, 133.164
12MP23-24
46
9737
2.3 18.0694
11.8
0.4761
12.3
12MP23-37
464
207521
1.2 18.4342
1.3
0.4726
1.7
12MP23-08
341
71150
2.0 18.1999
2.2
0.4832
2.7
12MP23-73
254
22741
2.5 17.7040
1.8
0.5004
2.4
12MP23-45
314
35373
1.3 17.5821
2.6
0.5127
2.7
12MP23-44
153
26819
1.0 18.0892
6.3
0.4984
6.4
12MP23-19
317
90392
1.1 18.1517
1.3
0.4979
2.6
12MP23-67
1054
724286
1.5 18.1170
0.7
0.5032
1.7
12MP23-32
163
33474
0.8 18.2235
4.0
0.5021
4.9
12MP23-63
105
17467
0.9 18.3556
6.0
0.4990
7.1
12MP23-64
36
7516
2.1 18.5963
23.1
0.4937
23.8
12MP23-40
113
22117
1.2 18.3027
5.5
0.5030
5.7
12MP23-02
478
85013
1.5 18.2023
1.4
0.5059
1.9
12MP23-97
399
135049
0.9 18.1829
1.1
0.5066
1.6
12MP23-51
96
22193
1.3 18.8499
7.0
0.4904
7.2
12MP23-16
275
58596
1.6 18.1192
2.2
0.5109
3.0
12MP23-09
181
59435
0.6 17.6967
4.0
0.5239
4.1
12MP23-58
196
59413
1.3 18.6839
3.9
0.4968
4.5
12MP23-04
100
32096
1.9 18.5067
8.5
0.5024
9.6
12MP23-15
450
104706
1.1 18.1622
1.4
0.5121
1.8
12MP23-22
90
19431
2.5 18.0963
6.8
0.5140
7.1
12MP23-71
273
118710
0.6 17.9908
2.3
0.5181
2.8
12MP23-47
1153
399196
2.2 18.0323
0.6
0.5183
0.8
12MP23-31
104
46756
3.6 18.6683
4.4
0.5008
5.9
12MP23-95
495
176115
1.5 17.9292
0.8
0.5225
2.1
12MP23-28
204
7952
1.1 17.7893
4.0
0.5275
4.2
12MP23-110
176
33819
1.5 18.3464
4.5
0.5122
4.8
12MP23-102
632
267417
1.1 18.1038
1.4
0.5202
1.9
12MP23-52
421
79497
1.3 18.1935
2.0
0.5193
2.2
12MP23-86
153
41271
2.4 18.4125
3.1
0.5141
4.7
12MP23-27
114
43426
2.1 18.9996
5.0
0.4993
5.2
12MP23-81
12MP23-91
12MP23-29
12MP23-85
12MP23-103
12MP23-30
12MP23-18
12MP23-108
12MP23-49
12MP23-93
12MP23-06
12MP23-10
12MP23-05
12MP23-39
12MP23-62
12MP23-99
12MP23-17
12MP23-11
12MP23-84
12MP23-70
12MP23-41
12MP23-104
12MP23-75
12MP23-92
12MP23-107
12MP23-79
12MP23-80
12MP23-72
12MP23-61
12MP23-57
12MP23-60
12MP23-105
12MP23-53
12MP23-23
12MP23-26
12MP23-96
12MP23-55
12MP23-25
12MP23-77
12MP23-56
12MP23-34
12MP23-83
12MP23-42
12MP23-98
12MP23-59
12MP23-12
12MP23-88
12MP23-50
12MP23-109
12MP23-101
12MP23-38
12MP23-14
87
68
106
114
85
77
45
132
228
181
130
97
81
188
165
317
89
99
133
456
598
83
135
220
249
189
391
194
345
101
38
110
425
694
726
63
53
62
99
32
102
698
217
128
135
64
124
51
235
634
91
28
20982
17453
17050
17109
13950
22744
9078
54025
64848
44557
31809
34205
6610
49823
68630
59274
14377
48927
27285
55564
194612
18645
41230
68031
225653
68219
117668
102874
105964
50214
10815
25543
173900
173433
275321
13976
11238
13440
21366
13156
18765
289964
42740
31186
39644
31878
65059
25674
105325
786305
52215
21194
2.7
1.5
2.4
1.1
1.6
2.6
2.8
1.6
2.9
1.4
3.3
2.0
2.9
2.6
2.2
2.1
2.0
1.8
1.3
1.7
1.7
2.8
2.7
1.7
1.6
2.7
2.7
1.9
4.8
2.6
3.0
2.5
1.2
0.4
1.7
2.3
1.4
0.6
3.0
2.1
2.0
0.5
1.6
1.5
1.7
1.4
1.0
2.2
9.4
54.6
1.1
2.6
18.8614
19.5108
18.9827
17.9819
18.6271
19.1747
19.0256
18.3227
18.0317
17.9591
17.3757
18.9543
17.4749
17.9877
18.0802
13.6024
18.2964
18.0494
18.1546
18.1644
17.8510
18.2712
18.0399
17.8132
17.8241
17.6607
18.2327
18.0882
17.8242
17.8759
17.1537
17.6561
17.8470
17.6682
17.7179
17.3468
18.1531
17.6222
18.4296
18.4056
17.7694
17.4550
17.0932
17.0363
16.9681
16.3032
15.9969
14.4261
14.0460
13.5726
13.4877
13.4631
8.2
11.8
6.1
4.1
3.7
9.3
12.5
5.2
2.2
1.6
4.7
6.7
4.6
3.0
3.5
2.0
3.8
4.6
6.0
0.9
1.1
6.8
3.6
3.4
1.7
3.2
2.0
4.6
1.7
5.2
14.8
6.3
1.5
0.6
0.8
8.5
11.1
7.1
7.0
14.7
3.5
0.8
2.1
5.6
4.4
5.9
2.3
2.9
0.6
0.3
1.9
7.4
0.5034
0.4869
0.5006
0.5285
0.5138
0.4994
0.5037
0.5242
0.5328
0.5352
0.5552
0.5094
0.5534
0.5377
0.5369
0.7138
0.5309
0.5388
0.5374
0.5385
0.5511
0.5395
0.5474
0.5558
0.5567
0.5622
0.5465
0.5509
0.5628
0.5687
0.6019
0.5881
0.5829
0.5901
0.5905
0.6299
0.6069
0.6273
0.6087
0.6146
0.6367
0.6518
0.6712
0.6952
0.7272
0.8410
0.9145
1.4933
1.5980
1.7821
1.7156
1.7519
8.5
11.9
6.4
4.2
4.4
9.5
12.7
5.5
2.9
2.1
4.8
6.9
4.8
3.8
3.8
4.3
4.1
5.2
6.6
2.3
1.3
7.3
4.3
3.9
2.3
3.5
2.3
5.2
1.8
5.4
15.3
7.3
2.8
1.2
1.3
10.6
11.3
7.3
7.1
14.9
3.8
1.5
4.9
5.8
5.3
6.0
2.7
4.2
1.4
0.9
4.7
7.7
12MP23-43
12MP23-33
12MP23-69
12MP23-66
12MP23-68
12MP23-106
12MP23-76
12MP23-54
12MP23-100
12MP23-74
12MP23-46
12MP23-94
12MP23-78
12MP23-48
12MP23-90
12MP23-13
12MP23-07
12MP23-03
12MP23-65
12MP23-36
12MP23-82
12MP23-89
145
496
410
40
44
98
50
636
72
50
133
85
159
155
164
95
30
72
18
15
154
81
74689
223194
217780
53696
29929
80573
35204
13409
59357
44409
244174
82624
263357
184870
41895
105016
61300
116178
21979
36320
289383
266791
1.4
1.3
4.3
2.1
3.4
1.6
0.8
3.2
1.3
1.1
15.0
2.0
1.4
1.9
1.0
1.3
0.4
0.9
1.2
1.6
5.3
1.2
13.3243
13.2470
13.2330
12.7046
12.4322
11.9727
10.7130
10.1083
10.0824
9.9915
9.9288
9.9244
9.7797
9.3092
9.0094
8.9687
8.9376
8.6852
7.2712
6.3640
5.4798
5.3662
1.1
0.5
0.4
4.8
2.5
1.4
1.3
0.8
1.0
1.6
0.5
1.2
0.2
0.6
0.8
0.5
2.2
0.9
1.5
2.6
0.3
0.5
1.8641
1.7138
1.8787
2.1745
2.2464
2.4285
3.3394
3.0536
3.9811
3.9329
3.9068
4.0212
4.1501
4.2358
4.7345
4.9210
4.9894
5.3715
7.3087
9.8734
12.2644
13.1001
1.9
1.3
1.2
5.7
3.3
28.2
2.0
2.2
1.3
1.8
1.9
2.2
1.2
3.9
13.0
1.5
2.6
1.5
2.7
3.6
1.8
1.6
12MP24; Yukon-Tanana, Port Houghton Assemblage, quartzite, (Degree Decimal: 57.31047, 133.19
12MP24-14
332
54731
0.7 18.3618
1.7
0.4455
9.1
12MP24-113
166
41352
1.2 18.1431
2.5
0.4624
7.1
12MP24-88
178
52359
1.2 18.1149
2.9
0.4687
3.4
12MP24-86
1962
165531
0.7 18.0320
0.6
0.4775
2.5
12MP24-32
368
115864
2.3 17.9535
1.4
0.4931
3.6
12MP24-111
295
35191
2.2 17.4987
3.3
0.5075
4.1
12MP24-04
478
172070
0.6 18.1055
1.1
0.4908
2.5
12MP24-48
461
147209
0.9 18.0460
0.8
0.4951
1.2
12MP24-69
354
146548
2.1 18.1077
1.7
0.4963
3.0
12MP24-85
161
48707
1.3 17.8845
3.1
0.5033
3.8
12MP24-10
210
50948
1.5 18.1715
1.4
0.4959
2.3
12MP24-22
282
20417
0.9 17.6517
2.8
0.5113
4.9
12MP24-115
266
111158
0.8 18.1037
1.6
0.4986
1.8
12MP24-01
177
58443
1.2 18.1078
3.1
0.4990
3.3
12MP24-96
490
163080
0.8 18.1116
0.5
0.4990
1.1
12MP24-58
177
44237
5.0 18.1399
3.2
0.5001
3.7
12MP24-73
321
79916
1.1 18.1354
1.8
0.5003
2.9
12MP24-122
192
76497
1.3 18.0774
3.1
0.5023
3.3
12MP24-61
432
199237
0.9 18.0816
0.5
0.5027
3.6
12MP24-77
359
87164
0.9 17.9049
3.3
0.5094
4.7
12MP24-103
336
149481
0.9 18.1398
1.5
0.5035
2.0
12MP24-64
357
86635
1.0 18.1843
2.0
0.5031
6.0
12MP24-105
140
38015
2.1 18.0577
2.6
0.5100
3.8
12MP24-18
225
113975
1.2 18.1355
1.6
0.5086
1.9
12MP24-81
454
255657
1.1 18.0917
1.2
0.5109
1.4
12MP24-90
495
208048
1.1 18.2086
1.0
0.5079
1.4
12MP24-20
552
115845
1.0 18.0349
1.8
0.5129
3.4
12MP24-15
147
52564
1.5 18.0359
3.0
0.5161
3.8
12MP24-94
12MP24-125
12MP24-91
12MP24-28
12MP24-121
12MP24-82
12MP24-117
12MP24-50
12MP24-56
12MP24-09
12MP24-35
12MP24-107
12MP24-102
12MP24-36
12MP24-97
12MP24-11
12MP24-84
12MP24-37
12MP24-31
12MP24-71
12MP24-21
12MP24-76
12MP24-23
12MP24-44
12MP24-110
12MP24-112
12MP24-78
12MP24-45
12MP24-40
12MP24-47
12MP24-114
12MP24-100
12MP24-83
12MP24-87
12MP24-123
12MP24-08
12MP24-116
12MP24-60
12MP24-65
12MP24-07
12MP24-106
12MP24-05
12MP24-43
12MP24-99
12MP24-92
12MP24-59
12MP24-98
12MP24-13
12MP24-27
12MP24-89
12MP24-24
12MP24-66
222
55
449
749
536
41
188
141
240
460
289
115
83
57
1140
188
229
132
179
117
607
116
288
196
179
230
299
156
101
485
67
422
479
108
219
281
41
239
69
66
43
375
287
229
546
370
702
724
169
76
87
107
55602
19468
140447
174205
176596
34748
65849
31221
55091
96200
280715
36004
36570
19598
414690
68028
101317
50275
50453
71868
119952
71065
28810
56853
84288
194128
68708
66975
239963
250382
41308
265251
105479
23860
102668
90429
24028
66280
24155
19083
22208
303329
79826
176686
152309
157033
215331
194210
35367
25282
69481
41805
0.7
1.9
1.2
0.4
1.1
1.5
2.2
2.7
2.4
1.4
1.7
2.0
1.9
1.7
0.8
1.8
1.9
1.6
1.4
2.2
1.3
4.8
2.1
1.7
2.2
2.8
2.7
2.1
2.0
2.0
2.2
1.7
1.1
1.9
1.6
1.4
2.6
1.2
2.9
2.0
2.4
3.9
1.4
1.2
18.3
1.2
0.9
1.0
1.3
1.9
1.0
1.2
18.1631
17.1863
18.1831
17.9715
18.0661
19.1086
17.8568
17.8331
18.1081
17.9383
18.0460
18.6006
17.7645
16.9877
18.0603
17.7709
18.3376
18.3321
18.0342
17.7613
17.9317
17.8106
17.8230
18.1326
17.8205
17.8598
17.9731
17.7539
17.3065
17.6918
17.7657
17.8145
17.9790
17.4908
17.5909
17.8592
18.1903
17.9294
17.8980
18.4857
18.2863
17.8578
17.7911
17.6929
17.7836
17.6272
17.6357
17.5509
17.0110
17.0750
16.9037
17.0747
1.8
9.1
1.2
0.6
0.7
20.7
1.9
3.9
2.7
1.6
1.3
4.9
4.1
15.2
0.5
2.9
1.6
3.4
3.2
5.0
0.7
3.5
2.4
1.3
3.0
2.0
1.9
2.6
3.9
1.0
7.1
1.1
1.1
5.4
1.7
1.7
7.6
2.1
4.1
5.5
7.4
1.5
1.7
2.2
0.8
1.2
0.8
0.6
2.3
4.1
3.5
2.6
0.5140
0.5437
0.5142
0.5216
0.5195
0.4912
0.5292
0.5305
0.5225
0.5280
0.5251
0.5098
0.5339
0.5602
0.5292
0.5384
0.5218
0.5225
0.5313
0.5399
0.5358
0.5408
0.5407
0.5348
0.5476
0.5476
0.5457
0.5580
0.5756
0.5650
0.5643
0.5631
0.5619
0.5777
0.5755
0.5668
0.5566
0.5668
0.5692
0.5537
0.5637
0.5818
0.5848
0.5904
0.5898
0.5961
0.6139
0.6219
0.6444
0.6590
0.7273
0.7273
3.9
9.3
5.3
1.7
1.2
20.9
2.5
4.2
2.7
2.0
1.5
5.5
4.6
15.6
1.8
3.0
1.7
3.6
3.5
5.1
1.2
4.0
2.5
1.8
3.5
2.2
2.3
3.4
4.2
1.7
7.1
1.8
2.2
5.6
2.1
2.4
7.9
2.7
4.5
6.0
7.9
2.0
2.6
2.7
1.5
1.8
1.3
0.9
2.9
4.4
4.0
4.0
12MP24-75
12MP24-63
12MP24-70
12MP24-62
12MP24-51
12MP24-25
12MP24-80
12MP24-120
12MP24-16
12MP24-46
12MP24-39
12MP24-54
12MP24-124
12MP24-53
12MP24-06
12MP24-34
12MP24-72
12MP24-03
12MP24-26
12MP24-41
12MP24-57
12MP24-55
12MP24-17
12MP24-109
12MP24-30
12MP24-49
12MP24-42
12MP24-67
12MP24-104
12MP24-02
12MP24-38
12MP24-119
12MP24-79
12MP24-101
12MP24-118
12MP24-12
12MP24-29
12MP24-33
12MP24-95
12MP24-19
78
299
58
207
104
241
180
19
36
144
222
76
334
132
52
143
54
253
68
191
163
37
138
42
107
74
125
89
130
217
186
49
42
35
71
45
42
124
174
87
26387
167049
22607
205298
77866
144511
92705
9220
15288
96827
85310
37813
170653
34879
42191
54843
57596
179805
152749
295201
72109
29080
150160
38673
79962
89144
172711
109582
268716
222221
189228
86065
74108
53255
113407
217141
85684
330012
258095
185091
0.9
1.1
1.2
1.2
1.1
0.8
0.9
1.8
1.2
1.3
2.1
1.5
2.1
1.0
0.6
3.3
1.0
1.7
1.1
2.4
12.8
2.3
2.0
0.9
1.8
2.6
2.0
1.1
1.4
0.9
5.6
1.0
0.8
1.5
0.6
0.8
0.5
1.7
1.7
1.4
16.9741
16.8611
17.2684
17.0192
17.0665
16.7781
17.0284
16.1112
16.7908
16.3977
16.3316
15.7025
16.3287
15.8013
14.2320
14.0980
13.9187
13.4771
13.2864
13.2506
12.9825
12.7830
12.7410
12.5477
11.4475
11.3773
10.9515
10.9296
10.0290
9.6263
9.2832
8.5829
8.1386
7.7685
5.8786
5.7639
5.7499
5.7296
4.8761
4.5569
2.7
0.9
2.5
1.3
3.6
1.7
1.7
14.5
7.3
3.0
1.1
3.8
0.9
2.6
3.2
1.3
3.3
0.5
1.8
0.6
1.2
4.5
1.1
2.3
0.6
1.4
0.7
1.3
0.9
0.3
1.1
0.8
1.0
0.8
0.4
0.5
0.6
0.2
0.3
0.3
0.7383
0.7489
0.7325
0.7434
0.7415
0.7573
0.7470
0.8149
0.7996
0.8315
0.8923
0.9501
0.9148
0.9813
1.4589
1.5647
1.5799
1.7912
1.8753
1.7928
2.2622
2.1423
2.0278
2.1589
2.7857
2.7891
3.1540
3.1462
3.7689
4.2531
3.1937
5.3960
6.1411
6.6190
11.3384
11.8289
10.9254
11.2727
14.6882
16.5173
2.9
1.2
2.8
1.8
3.7
2.0
1.9
15.1
7.6
3.1
2.8
4.5
4.4
7.0
3.4
2.1
3.6
1.0
4.1
1.9
11.9
4.8
2.2
4.1
1.9
1.5
1.3
1.7
2.4
1.5
3.6
2.0
2.1
1.6
0.8
1.4
1.3
2.8
2.8
1.5
12MP25; Yukon-Tanana, Port Houghton Assemblage, quartzite, (Degree Decimal: 57.30333, 133.23
12MP25-94
595
56444
0.9 18.1754
1.1
0.3704
6.5
12MP25-34
153
36512
2.2 18.2083
5.3
0.3842
6.1
12MP25-14
512
22981
1.8 17.7274
3.3
0.4733
6.8
12MP25-53
1101
177879
1.2 18.1211
0.5
0.4780
1.5
12MP25-10
141
29586
2.3 19.1465
3.6
0.4565
3.9
12MP25-38
147
15938
1.8 17.7702
4.4
0.5003
7.0
12MP25-78
364
109088
1.1 17.9643
1.2
0.4996
3.2
12MP25-58
197
63430
1.7 17.1441
9.5
0.5237
9.8
12MP25-15
1002
279515
0.6 18.0718
0.5
0.4974
1.3
12MP25-91
1443
216812
0.9 18.0752
0.4
0.4982
2.0
12MP25-72
12MP25-40
12MP25-42
12MP25-84
12MP25-46
12MP25-26
12MP25-08
12MP25-98
12MP25-100
12MP25-02
12MP25-33
12MP25-101
12MP25-51
12MP25-52
12MP25-48
12MP25-61
12MP25-18
12MP25-R33
12MP25-R33
12MP25-62
12MP25-41
12MP25-32
12MP25-12
12MP25-59
12MP25-57
12MP25-102
12MP25-79
12MP25-97
12MP25-69
12MP25-31
12MP25-49
12MP25-07
12MP25-39
12MP25-71
12MP25-21
12MP25-65
12MP25-11
12MP25-35
12MP25-63
12MP25-76
12MP25-20
12MP25-77
12MP25-66
12MP25-96
12MP25-29
12MP25-47
12MP25-06
12MP25-89
12MP25-93
12MP25-27
12MP25-28
12MP25-19
360
202
1097
405
285
105
221
186
217
183
241
67
67
54
255
691
107
303
64
59
247
184
229
52
175
46
207
423
113
173
99
145
66
564
147
197
292
292
106
1131
334
190
157
320
211
300
71
110
262
159
281
97
73158
57174
316253
126173
66668
28789
46726
32635
73115
76635
70729
27543
32255
10589
86939
248419
31799
71798
19705
13173
79986
43213
127263
16045
64752
19289
38523
199971
67277
149697
47884
64439
23317
354686
39565
56768
208765
132512
26839
219044
54836
90402
66395
304881
49781
71873
49070
35859
78697
67024
190688
35227
1.6
1.7
1.1
1.1
1.1
1.8
1.2
3.2
1.4
1.2
0.6
1.7
1.4
2.5
1.8
1.7
2.2
1.4
1.6
3.3
1.7
2.0
2.6
2.4
2.9
2.8
1.8
1.2
2.2
3.0
1.4
1.6
1.5
1.8
1.5
2.4
2.2
2.1
2.5
1.2
1.9
1.3
2.5
2.6
2.5
1.6
1.9
3.8
3.8
1.0
1.5
2.0
18.0928
18.3200
18.0105
18.2322
17.8461
18.0126
18.3195
17.5832
17.7948
17.4627
18.0719
18.5686
17.3690
17.2751
17.8719
17.7241
17.8921
18.1859
18.1348
17.3802
18.0189
18.3821
17.8637
19.3758
18.1275
18.0849
17.5493
17.8201
17.8105
17.7397
17.6895
17.8055
18.2547
17.9255
18.5533
17.9679
17.7914
17.8170
18.2781
17.8281
17.3516
17.8010
17.9146
17.7693
17.7277
17.3514
17.4152
18.4821
17.8522
17.1719
17.6435
17.3616
1.6
1.6
0.5
1.3
2.5
4.1
2.3
4.3
2.1
3.7
2.6
9.3
10.0
6.1
1.9
0.8
5.8
1.6
6.3
11.6
2.2
1.3
3.7
13.5
4.6
9.6
2.6
1.6
4.7
2.7
5.5
3.3
7.7
1.0
5.3
3.0
1.5
1.8
3.2
0.5
0.9
3.4
3.0
2.0
2.4
1.9
5.2
4.4
2.2
3.0
1.6
2.9
0.4987
0.4935
0.5020
0.4962
0.5145
0.5113
0.5041
0.5273
0.5234
0.5343
0.5167
0.5034
0.5382
0.5415
0.5236
0.5282
0.5233
0.5153
0.5175
0.5426
0.5234
0.5132
0.5291
0.4881
0.5220
0.5245
0.5408
0.5337
0.5364
0.5388
0.5429
0.5406
0.5288
0.5387
0.5228
0.5422
0.5500
0.5511
0.5373
0.5516
0.5687
0.5574
0.5566
0.5620
0.5657
0.5838
0.5856
0.5550
0.6025
0.6267
0.6141
0.6431
1.8
1.9
1.0
1.5
2.7
4.4
2.5
6.2
3.2
4.1
3.1
9.4
10.2
8.1
2.3
1.2
5.8
1.8
6.8
12.0
3.0
1.6
4.2
13.8
4.7
10.4
3.5
1.9
5.7
2.9
7.3
3.4
7.9
1.4
5.5
3.2
2.9
2.5
3.9
1.4
2.3
4.4
3.2
2.9
2.6
2.5
5.4
4.6
2.9
3.4
2.1
3.3
12MP25-17
12MP25-37
12MP25-87
12MP25-16
12MP25-05
12MP25-55
12MP25-13
12MP25-43
12MP25-83
12MP25-54
12MP25-86
12MP25-22
12MP25-75
12MP25-60
12MP25-25
12MP25-90
12MP25-24
12MP25-36
12MP25-68
12MP25-99
12MP25-103
12MP25-09
12MP25-23
12MP25-44
12MP25-64
12MP25-50
12MP25-82
190
41
55
74
69
387
30
123
107
284
274
418
87
28
228
48
89
138
75
36
14
51
38
316
222
18
155
61172
27812
20071
60478
10213
254688
21023
64335
11627
86089
532791
678498
104423
34453
223521
107150
195655
123981
75301
8324
31949
57833
144318
319976
330626
31895
345299
1.0
1.6
2.0
1.9
1.3
0.8
1.8
1.0
0.3
1.6
1.4
3.1
2.4
2.2
2.6
0.7
1.5
1.9
1.1
1.1
2.4
1.0
1.7
1.7
0.5
1.2
1.2
17.1545
17.6905
17.5144
16.7588
16.1252
16.8988
18.5366
16.5779
16.5025
16.6255
14.5351
13.5754
12.8364
12.7756
12.6626
12.6285
11.5073
10.9218
10.5214
9.6357
9.5978
9.4958
9.4541
8.7272
8.7071
7.3692
6.4113
1.6
10.5
8.0
6.7
5.3
1.2
18.9
2.8
3.0
1.6
1.1
0.3
1.4
4.6
0.9
2.5
1.7
0.9
1.5
6.5
4.3
1.2
1.0
0.2
0.3
2.2
0.4
0.6549
0.6354
0.6437
0.6854
0.7307
0.7241
0.6688
0.7601
0.7744
0.7796
1.3477
1.6860
2.0633
2.0413
2.1661
2.1521
2.7826
3.1646
3.4025
3.9423
4.2240
4.4427
4.5059
5.0483
4.8624
6.9032
8.8451
1.9
10.7
8.7
6.9
7.5
1.9
19.2
5.1
3.8
3.4
4.5
0.8
2.1
4.7
1.5
3.0
2.3
1.6
1.9
7.0
4.9
1.8
1.3
0.6
2.1
3.8
1.6
12MP33; Yukon-Tanan, Tracy Arm Assemblage, orthoquartzite, (Degree Decimal: 57.89338, 133.29
12MP33-08
178
16258
1.5 19.0199
7.4
0.1858
9.0
12MP33-42
331
12568
20.1 18.7501
4.9
0.2342
9.3
12MP33-53
161
21867
9.1 10.7984
5.2
0.4631
10.3
12MP33-72
993
7358
1.8 13.6264
2.4
0.5299
6.9
12MP33-58
1214
15483
3.3 13.0631
1.9
0.5703
4.3
12MP33-48
514
38176
4.3 12.2123
1.5
0.6243
8.7
12MP33-54
1004
9760
8.7 13.1288
0.8
0.6525
2.9
12MP33-02
616
78899
7.4 12.4300
3.1
0.8070
6.5
12MP33-27
715
6508
25.1 12.7454
2.7
0.8650
3.9
12MP33-04
129
68463
2.3 13.2688
1.5
1.8677
2.8
472
12737
10.6 11.7177
2.5
0.9640
4.2
12MP33-80
12MP33-03
415
15580
4.1 11.0910
2.1
0.9238
8.8
12MP33-98
144
69293
1.0
9.4094
0.4
3.6435
1.5
12MP33-90
285
105640
2.7
9.3801
0.6
3.9682
9.3
12MP33-66
211
56868
2.6
9.3680
0.9
4.2114
4.9
12MP33-62
109
67778
1.3
9.3282
0.8
3.8329
3.6
12MP33-77
173
80785
2.2
9.2496
0.6
4.2310
5.0
12MP33-16
190
118125
6.8
9.2479
0.4
3.7618
3.8
12MP33-86
184
150685
2.2
9.2470
0.3
3.9800
2.5
12MP33-79
222
139372
2.8
9.2369
0.3
4.2369
6.1
12MP33-37
120
207674
1.2
9.2304
0.7
4.5875
2.9
12MP33-57
189
106362
1.3
9.2177
0.5
4.4222
1.4
12MP33-22
88
145004
2.1
8.9744
0.7
4.2420
3.0
12MP33-103
12MP33-32
12MP33-26
12MP33-23
12MP33-69
12MP33-71
12MP33-85
12MP33-102
12MP33-47
12MP33-24
12MP33-87
12MP33-67
12MP33-30
12MP33-56
12MP33-92
12MP33-31
12MP33-68
12MP33-46
12MP33-76
12MP33-40
12MP33-39
12MP33-100
12MP33-83
12MP33-33
12MP33-29
135
62
103
146
77
75
88
136
218
168
176
73
134
178
120
537
114
125
188
110
101
133
61
77
18
141610
72764
115507
214458
158050
63820
58995
116719
403322
239133
112011
69289
105375
202929
90800
32018
61488
84349
82571
62102
81497
57156
147844
411517
23997
1.8
1.5
1.1
2.3
14.1
0.5
0.9
1.3
0.7
1.3
3.8
0.5
3.1
2.0
2.4
3.0
1.0
2.2
2.7
2.9
2.0
2.0
2.3
0.8
4.5
8.9605
8.9231
8.8961
8.8935
8.8264
8.8177
8.8110
8.7917
8.7186
8.7175
8.5110
8.3535
7.8289
7.6054
7.4984
7.3375
6.3722
6.1200
6.0101
5.8886
5.7159
5.5303
5.4976
5.4780
5.4757
0.3
1.4
0.7
0.5
0.7
1.1
0.9
0.4
0.4
0.8
0.7
0.7
0.5
0.5
0.4
1.5
0.4
0.3
0.3
0.3
0.8
0.3
0.4
0.6
3.3
4.1577
4.7094
5.3158
4.6317
4.6971
5.0554
5.0605
4.6229
4.7418
4.2864
4.6870
5.2515
5.7848
6.5850
6.6522
1.4173
9.0395
8.9640
9.7833
10.0764
11.1149
9.8722
12.1240
10.9420
11.8819
4.7
2.5
8.2
1.4
2.9
1.5
1.2
1.8
4.1
9.1
6.8
2.4
1.9
3.8
1.7
6.4
2.7
1.5
2.2
1.1
1.5
4.9
3.4
3.2
8.0
12MP38; Yukon-Tanana, Port Houghton Assemblage, basal conglomerate, (Degree Decimal: 57.96
12MP38-73
557
32240
1.8 18.6343
1.3
0.3688
3.1
12MP38-77
300
53685
2.2 18.4335
2.5
0.3842
5.7
12MP38-42
585
16283
2.5 18.5007
1.2
0.3893
2.6
12MP38-12
155
49444
3.4 18.8782
3.2
0.3908
10.0
12MP38-19
227
51370
2.8 18.7063
2.5
0.3961
2.7
12MP38-35
689
64646
2.0 18.6810
1.3
0.3983
5.2
12MP38-72
212
63633
2.9 18.7993
3.5
0.3974
3.9
12MP38-01
160
95587
1.5 18.4201
3.3
0.4098
5.5
12MP38-32
584
48654
1.8 18.8278
1.5
0.4013
2.3
12MP38-63
272
82396
1.8 19.0612
1.6
0.3967
2.5
12MP38-52
215
61952
2.1 18.7226
2.9
0.4048
3.2
12MP38-45
108
49130
3.5 18.7151
5.5
0.4051
6.3
12MP38-71
283
90855
2.3 18.5825
1.5
0.4081
1.8
12MP38-88
227
56549
3.2 18.9101
3.3
0.4011
3.8
12MP38-24
133
48989
2.6 19.0096
6.6
0.3992
6.8
12MP38-18
320
145991
2.2 18.4985
2.8
0.4107
3.0
12MP38-37
178
152118
3.1 18.6593
1.8
0.4076
2.3
12MP38-25
190
84351
3.5 18.4274
2.6
0.4128
2.7
12MP38-08
397
110127
1.7 18.7668
1.2
0.4054
1.8
12MP38-87
206
87597
2.8 18.6351
2.0
0.4084
2.3
12MP38-22
226
86149
3.3 18.5602
2.4
0.4102
2.6
12MP38-58
279
118620
2.0 18.7138
2.6
0.4070
3.0
12MP38-40
232
105075
1.8 18.3421
2.2
0.4153
3.0
12MP38-97
292
62959
2.6 18.4046
1.6
0.4142
3.5
12MP38-41
156
185069
3.6 18.1637
3.9
0.4197
4.1
12MP38-20
12MP38-31
12MP38-29
12MP38-30
12MP38-93
12MP38-38
12MP38-49
12MP38-02
12MP38-55
12MP38-21
12MP38-05
12MP38-70
12MP38-74
12MP38-59
12MP38-79
12MP38-66
12MP38-53
12MP38-17
12MP38-39
12MP38-85
12MP38-44
12MP38-27
12MP38-51
12MP38-10
12MP38-11
12MP38-69
12MP38-102
12MP38-64
12MP38-75
12MP38-99
12MP38-68
12MP38-14
12MP38-26
12MP38-92
12MP38-15
12MP38-36
12MP38-57
12MP38-61
12MP38-06
12MP38-105
12MP38-104
12MP38-81
12MP38-86
12MP38-16
12MP38-80
12MP38-65
12MP38-91
12MP38-56
12MP38-33
12MP38-101
12MP38-50
12MP38-62
198
179
224
208
202
143
233
239
237
159
172
201
187
204
142
349
108
249
183
171
163
190
114
136
187
245
202
183
283
201
207
168
191
240
183
170
98
141
211
229
144
282
199
162
182
385
537
168
99
173
114
165
115289
68503
85377
40387
44678
52155
83824
155966
245782
72422
85365
60987
87676
67601
63709
119690
32340
151782
70979
109899
100526
75552
82308
28207
63030
53849
151782
64010
67589
87593
27788
36841
36227
46031
62066
86488
33719
42376
65103
77851
44932
104610
64067
40210
86746
94857
66212
50383
50185
70981
123959
43899
1.9
2.8
2.4
2.2
2.2
3.2
2.3
3.3
2.9
3.2
3.0
2.3
2.6
1.9
3.0
1.4
2.9
3.5
2.3
2.9
1.6
2.4
3.0
4.1
3.2
2.8
2.2
3.2
2.5
2.4
2.6
3.3
3.6
2.0
2.5
3.2
2.7
3.1
2.1
2.2
3.6
2.6
1.7
3.4
3.3
1.8
1.7
2.2
2.8
2.7
3.6
3.5
19.0181
18.9470
18.6837
19.1069
18.7951
19.2553
18.8231
19.1142
18.7827
18.5818
18.7483
18.6165
18.7635
18.5117
18.7438
18.5556
17.9512
18.7543
18.6710
18.6062
18.9798
18.6177
18.2651
19.4431
18.7629
18.6342
18.2724
18.5394
18.8039
19.2536
18.9138
18.4128
18.8341
18.1589
18.3199
18.5852
18.6441
18.9570
18.6018
18.7159
19.3726
18.5588
19.1480
19.1388
19.1228
18.5785
18.6668
18.5620
18.5925
18.3469
18.2102
18.9332
2.1
4.7
2.0
2.2
3.6
6.5
2.4
2.3
3.2
3.3
2.7
4.1
2.4
1.6
2.3
1.4
7.2
2.2
3.4
4.2
2.2
3.2
6.5
5.1
5.1
1.9
2.5
2.3
2.7
3.2
2.8
2.6
2.7
3.6
3.6
2.8
5.0
2.8
1.9
2.3
5.7
1.1
4.0
2.7
2.8
1.3
1.7
1.9
6.2
2.8
3.9
4.4
0.4010
0.4026
0.4084
0.3997
0.4064
0.3968
0.4059
0.3998
0.4070
0.4115
0.4080
0.4110
0.4079
0.4136
0.4090
0.4132
0.4272
0.4089
0.4108
0.4124
0.4049
0.4128
0.4210
0.3957
0.4101
0.4129
0.4212
0.4153
0.4095
0.4000
0.4073
0.4187
0.4093
0.4248
0.4210
0.4150
0.4141
0.4075
0.4154
0.4132
0.3995
0.4172
0.4046
0.4049
0.4052
0.4172
0.4154
0.4179
0.4181
0.4238
0.4272
0.4115
3.5
5.0
2.3
2.3
5.6
6.6
2.6
2.7
3.8
3.5
4.1
4.5
3.7
2.9
2.5
1.9
7.3
2.3
3.6
4.3
2.4
3.4
6.6
5.2
5.4
2.2
3.0
2.7
3.0
3.4
3.1
3.6
3.0
5.2
3.7
3.2
5.6
2.9
2.3
2.5
5.8
1.4
4.3
2.8
3.0
1.9
2.8
2.2
6.4
3.2
5.1
4.5
12MP38-76
12MP38-100
12MP38-90
12MP38-23
12MP38-98
12MP38-78
12MP38-43
12MP38-48
12MP38-60
12MP38-103
12MP38-46
12MP38-09
12MP38-94
12MP38-07
12MP38-03
12MP38-34
12MP38-54
12MP38-89
12MP38-84
12MP38-47
12MP38-83
12MP38-96
251
135
196
152
150
171
149
363
242
127
140
255
951
150
213
286
117
261
24
88
257
105
98640
59310
56024
49849
113599
54175
41141
92260
92044
73357
48829
7798
82072
31772
35673
347184
185824
38964
66847
179240
145567
531862
1.9
2.8
2.1
2.8
3.6
3.8
2.6
2.6
1.8
3.0
3.2
2.4
1.2
2.7
3.3
1.8
1.1
3.8
0.4
1.6
1.9
2.2
18.5044
18.3132
18.7992
18.6713
18.6563
19.0445
18.8116
18.7020
18.6624
18.6312
19.1573
18.0303
18.5938
18.9011
18.7628
11.6369
9.8603
9.2263
8.9219
8.4685
7.1699
5.2548
2.5
4.1
4.5
2.7
4.0
3.2
2.2
1.7
2.3
5.7
3.7
3.9
0.5
2.6
3.3
0.3
0.4
0.2
1.5
0.6
1.3
0.4
0.4211
0.4259
0.4149
0.4180
0.4184
0.4099
0.4153
0.4183
0.4195
0.4202
0.4087
0.4364
0.4232
0.4193
0.4532
2.6454
4.1098
4.0445
5.0632
5.6717
6.9257
14.0450
6.3
4.5
5.1
2.9
4.1
4.7
4.2
2.0
5.5
5.9
3.9
4.5
1.0
3.1
9.3
1.8
2.1
5.4
2.1
1.0
1.8
0.9
12MP39; Yukon-Tanana, Port Houghton Assemblage, basal conglomerate, (Degree Decimal: 57.94
12MP39-04
227
103778
1.3 18.5755
2.3
0.4052
2.9
12MP39-03
160
22893
2.3 19.1241
4.1
0.3954
4.1
12MP39-68
398
114166
1.7 18.6067
1.3
0.4072
1.5
12MP39-60
73
27257
1.9 17.5689
7.3
0.4318
7.7
12MP39-33
169
133589
2.1 18.8380
4.7
0.4033
6.0
12MP39-36
513
53434
1.9 18.6124
1.2
0.4087
1.8
12MP39-61
94
35323
1.9 18.3137
9.1
0.4167
9.2
12MP39-86
128
40232
3.5 18.2247
5.4
0.4190
5.6
12MP39-02
741
145541
1.4 18.7098
1.3
0.4087
1.9
12MP39-58
282
57827
1.1 18.7397
3.2
0.4085
3.5
12MP39-41
144
46539
2.6 19.3577
4.7
0.3960
4.8
12MP39-17
331
51130
1.9 18.8523
1.2
0.4067
1.5
12MP39-48
241
41026
2.3 18.6389
3.2
0.4118
3.3
12MP39-71
262
83560
2.1 18.5791
2.4
0.4132
2.6
12MP39-96
138
47819
2.9 18.7244
4.9
0.4110
6.7
12MP39-21
457
77850
1.1 18.4788
1.7
0.4170
3.0
12MP39-44
173
39081
2.0 18.7816
4.0
0.4106
4.7
12MP39-52
478
106974
1.0 18.6801
1.8
0.4143
2.1
12MP39-64
151
61261
1.8 18.4815
4.5
0.4187
4.6
12MP39-01
562
124439
2.1 18.6988
1.3
0.4146
1.5
12MP39-105
247
45216
1.7 18.4151
2.4
0.4219
3.3
12MP39-31
181
72034
1.6 18.8793
4.0
0.4121
4.5
12MP39-49
219
48868
1.9 18.7919
2.7
0.4145
5.1
12MP39-27
281
83115
1.9 18.6171
1.6
0.4185
1.9
12MP39-46
232
65812
2.0 18.8220
1.6
0.4152
1.9
12MP39-97
301
198854
2.0 18.8458
1.3
0.4157
2.1
12MP39-109
195
33091
1.5 18.5543
3.1
0.4228
3.4
12MP39-99
234
92358
1.8 18.6150
1.7
0.4223
2.2
12MP39-14
12MP39-24
12MP39-79
12MP39-15
12MP39-87
12MP39-80
12MP39-78
12MP39-13
12MP39-20
12MP39-54
12MP39-74
12MP39-90
12MP39-37
12MP39-08
12MP39-100
12MP39-63
12MP39-76
12MP39-16
12MP39-88
12MP39-82
12MP39-29
12MP39-89
12MP39-51
12MP39-91
12MP39-98
12MP39-69
12MP39-57
12MP39-92
12MP39-77
12MP39-35
12MP39-47
12MP39-94
12MP39-103
12MP39-72
12MP39-39
12MP39-55
12MP39-25
12MP39-23
12MP39-19
12MP39-56
12MP39-28
12MP39-11
12MP39-104
12MP39-101
12MP39-43
12MP39-65
12MP39-85
12MP39-95
12MP39-110
12MP39-59
12MP39-45
12MP39-84
298
198
170
126
494
595
45
446
88
48
252
64
105
41
37
19
113
152
93
95
99
78
52
22
61
97
156
201
116
365
87
60
46
37
73
125
197
47
29
16
78
48
36
101
27
17
23
44
56
168
18
110
36945
63786
65223
57793
270887
146157
12852
118188
30990
11952
198855
86228
75157
40983
25090
38941
216199
149295
246778
269089
152075
86044
87486
51466
87152
157899
277090
391627
207406
64292
39441
98203
84925
85850
175845
361909
255354
56350
53757
20456
128060
96845
70948
140160
100017
35727
154960
293339
250179
255405
63745
301600
1.8
2.7
2.6
1.2
2.8
1.9
1.9
1.6
1.7
3.0
0.8
2.1
2.5
1.7
2.0
2.4
1.9
2.4
2.0
0.9
1.9
0.8
1.3
1.1
1.5
1.4
1.4
2.1
1.2
4.7
1.2
1.1
2.3
1.2
1.1
1.3
3.4
1.1
0.7
1.2
2.8
1.5
1.7
1.2
0.9
0.4
1.6
0.3
1.4
1.5
0.1
1.4
17.9802
18.3818
18.4752
18.8257
18.5346
18.4486
20.3114
18.6950
18.7002
18.7451
16.0175
13.2086
13.1640
12.8020
12.6800
12.1748
11.6872
11.5303
11.3066
9.9592
9.9523
9.8902
9.7763
9.3958
9.2160
9.2140
9.1711
9.1616
9.1612
9.1185
9.0376
8.9657
8.9276
8.9114
8.8973
8.8856
8.8818
8.8673
8.8471
8.8206
8.8060
8.7898
8.7616
8.7188
8.6999
8.6412
8.6079
8.5273
8.4659
8.4479
8.4296
8.1827
3.2
3.0
3.1
4.6
1.0
0.7
13.6
1.4
6.3
7.6
0.9
1.7
1.2
2.0
3.7
5.1
0.7
0.5
1.7
0.8
0.5
1.2
1.7
1.9
1.1
0.7
0.4
0.5
0.5
0.1
0.7
0.7
0.8
1.5
0.9
0.3
0.2
1.4
1.3
1.3
0.5
1.2
1.3
0.7
2.6
2.6
3.9
0.6
0.6
0.4
2.2
0.5
0.4375
0.4282
0.4303
0.4234
0.4311
0.4337
0.3946
0.4341
0.5058
0.5074
0.9176
1.8757
1.8786
2.1003
2.1671
2.4942
2.7042
2.6507
2.9215
3.9651
3.8549
3.8471
4.0218
4.5817
4.7991
4.7012
4.7048
4.8429
4.7602
4.5546
4.7661
4.9883
5.1581
5.1290
5.2541
5.2524
5.1911
5.1308
5.0840
5.1050
5.0372
5.1492
5.4434
5.2134
5.1921
5.5128
5.5235
5.5818
5.6320
5.6093
5.6746
6.1540
3.8
3.6
3.3
4.7
3.4
1.2
13.9
3.2
6.8
7.8
1.5
2.2
1.6
2.8
4.2
5.6
2.1
3.5
2.3
1.3
2.2
2.5
2.4
2.7
1.4
1.0
1.4
1.0
1.2
0.8
1.8
1.5
2.6
1.8
2.0
2.3
1.1
2.1
2.7
3.0
1.6
2.6
1.9
1.3
3.7
3.5
4.1
1.5
1.7
1.6
2.5
1.2
12MP39-09
12MP39-07
12MP39-22
12MP39-81
12MP39-108
12MP39-50
12MP39-18
12MP39-26
12MP39-34
12MP39-05
12MP39-42
12MP39-66
12MP39-12
12MP39-93
12MP39-83
12MP39-106
12MP39-70
12MP39-107
12MP39-06
12MP39-10
12MP39-73
12MP39-52
12MP39-40
12MP39-32
12MP39-30
87
24
56
19
16
147
79
70
68
162
19
47
62
37
72
24
34
98
88
149
192
49
47
130
70
176296
53314
43569
42112
28500
274304
518360
141846
117546
33451
42843
48895
171683
119396
162338
245196
92259
378316
468655
619740
511011
139885
175648
435842
221753
1.0
1.0
0.9
1.2
0.9
1.7
1.2
1.7
1.4
1.3
0.6
1.5
2.0
0.7
1.5
0.8
1.4
2.6
0.6
0.7
0.6
1.1
1.1
0.7
0.9
8.1426
8.1339
7.7872
7.4020
7.0817
6.7529
6.6895
6.5336
6.4646
6.1443
6.1416
5.7382
5.7339
5.7036
5.4902
5.4191
5.3159
5.1866
4.5828
4.5814
4.5806
4.5805
4.5805
4.5791
3.8803
0.6
2.3
2.5
1.4
2.1
0.3
0.5
2.0
0.4
0.3
1.4
1.2
0.5
0.8
0.4
0.5
0.6
0.5
0.1
0.1
0.1
0.3
0.5
0.1
0.4
6.0926
6.1346
6.8201
7.4665
8.0676
8.8964
8.9965
8.7247
9.4649
8.7292
10.5666
11.7792
11.9702
11.9300
12.2704
12.8865
13.5451
13.9927
17.4531
18.0552
17.8448
17.6896
17.5273
17.9360
22.6751
1.5
3.1
2.7
2.1
3.5
1.0
2.4
5.0
2.7
6.7
1.6
2.3
4.4
1.6
1.4
1.8
2.8
1.6
0.9
0.9
0.9
3.6
2.7
0.8
1.9
12MP40; Yukon-Tanana, Endicott Arm Assemblage, orthoquartzite, (Degree Decimal: 58.05701, 13
12MP40-IC-108
92
9223
1.7 20.9971
3.7
0.0541
4.1
12MP40-IC-143
193
7728
2.9 21.0868
3.8
0.0543
3.9
12MP40-IC-113
72
6890
1.4 20.3258
3.1
0.0568
3.3
12MP40-55
478
20737
1.7 21.4920
1.1
0.0541
1.5
12MP40-IC-122
647
52282
1.0 21.4285
1.4
0.0545
3.0
12MP40-41
57
3831
1.7 21.0191
1.4
0.0560
2.1
12MP40-IC-115
441
22692
1.7 21.6702
1.2
0.0550
2.3
12MP40-IC-107
174
8982
1.9 21.2515
2.2
0.0561
2.4
12MP40-40
431
47459
2.6 21.3667
1.4
0.0564
3.1
12MP40-IC-111
260
10077
1.6 21.2829
1.6
0.0571
2.5
12MP40-IC-134
662
36270
2.7 21.1556
1.6
0.0600
2.0
487
31884
1837.4 18.2951
1.5
0.0695
2.2
12MP40-IC-124
12MP40-29
437
64999
1.0 21.0544
1.1
0.0616
5.5
12MP40-IC-109
249
10627
2.4 20.7793
1.3
0.0682
3.4
12MP40-IC-141
274
34640
1.1 20.8555
1.7
0.0700
2.3
12MP40-36
195
31375
3.6 20.8359
2.1
0.0712
2.7
12MP40-IC-120
264
14511
8.8 21.0163
1.7
0.0716
1.8
12MP40-48
286
29635
1.0 21.2033
1.1
0.0710
1.7
12MP40-31
726
133261
2.5 21.1797
0.7
0.0728
1.1
12MP40-IC-136
139
8852
2.4 20.9122
1.5
0.1025
2.2
12MP40-102
149
12029
1.4 21.0972
1.3
0.1077
1.9
12MP40-33
711
164656
1.5 20.5461
0.6
0.1259
7.4
12MP40-IC-137
207
29347
2.3 20.1637
1.9
0.1632
2.5
12MP40-51
274
59322
1.4 20.5310
1.0
0.1624
1.0
12MP40-IC-152
31
5967
2.6 20.0539
2.1
0.2314
2.8
12MP40-IC-123
12MP40-IC-114
12MP40-IC-144
12MP40-IC-132
12MP40-IC-155
12MP40-IC-140
12MP40-92
12MP40-88
12MP40-78
12MP40-86
12MP40-98
12MP40-IC-153
12MP40-23
12MP40-63
12MP40-64
12MP40-14
12MP40-IC-128
12MP40-10
12MP40-80
12MP40-61
12MP40-IC-119
12MP40-67
12MP40-68
12MP40-IC-151
12MP40-1
12MP40-70
12MP40-16
12MP40-IC-130
12MP40-IC-154
12MP40-IC-149
12MP40-IC-148
12MP40-20
12MP40-IC-127
12MP40-91
12MP40-IC-150
12MP40-IC-145
12MP40-IC-106
12MP40-11
12MP40-IC-146
12MP40-99
12MP40-2
12MP40-79
12MP40-28
12MP40-87
12MP40-38
12MP40-103
12MP40-77
12MP40-30
12MP40-6
12MP40-IC-125
12MP40-IC-112
12MP40-84
51
346
822
403
211
462
148
329
270
204
210
148
273
498
242
236
396
680
301
315
412
294
367
269
168
608
414
298
150
322
160
121
213
182
260
356
220
285
198
203
103
206
358
414
276
218
158
164
152
144
133
167
21152
68225
377418
148658
148137
148518
76597
104835
120209
88320
87433
30594
82999
261152
164976
174146
118638
360007
83349
190031
227047
327450
192673
134342
78154
282102
216325
249279
42657
147268
67058
44686
70935
130852
60835
237743
131553
242749
59875
149814
44907
38127
208685
308162
47195
301284
56770
407940
179366
38900
57994
75840
3.0
0.8
1.1
1.5
1.3
1.2
1.8
1.8
1.4
1.7
1.8
1.8
1.4
1.5
1.1
2.3
1.2
1.1
2.1
0.8
1.1
1.5
1.9
1.7
1.7
1.0
1.1
1.9
2.0
1.4
2.7
1.8
1.8
1.8
2.0
1.2
2.0
1.6
1.4
2.2
2.6
1.9
1.7
1.8
1.5
1.5
2.5
1.4
2.6
2.4
2.4
2.3
19.6891
18.5339
18.2382
18.3956
18.3450
18.3816
18.7145
18.5251
18.5085
18.7306
18.4695
18.3764
18.4565
18.5156
18.5278
18.4812
18.5087
18.4881
18.4561
18.5626
18.5824
18.3636
18.3225
18.5206
18.4564
18.3065
18.5038
18.3418
18.3574
18.4496
18.6053
18.4631
18.6162
18.5346
18.5329
18.3901
18.2880
18.5360
18.4912
18.4362
18.4725
18.5821
18.4300
18.4955
18.5652
18.4687
18.6132
18.2835
18.4481
18.3742
18.3828
18.4811
2.0
0.8
0.9
0.6
0.9
0.9
1.0
0.7
0.6
0.9
0.7
1.0
0.5
1.0
0.7
0.9
0.9
1.6
0.9
0.8
0.6
0.6
1.0
0.6
0.7
1.4
0.5
0.7
0.9
0.8
0.8
0.7
0.8
1.0
0.6
0.6
0.7
0.5
0.9
0.9
0.5
0.7
0.8
0.9
0.7
1.7
0.7
1.1
0.7
1.2
1.1
0.7
0.2450
0.3613
0.3824
0.3891
0.3971
0.3990
0.3952
0.4122
0.4148
0.4119
0.4181
0.4203
0.4188
0.4198
0.4206
0.4234
0.4231
0.4251
0.4269
0.4253
0.4256
0.4311
0.4323
0.4295
0.4316
0.4355
0.4321
0.4362
0.4368
0.4349
0.4319
0.4357
0.4332
0.4353
0.4361
0.4398
0.4427
0.4369
0.4392
0.4405
0.4397
0.4372
0.4410
0.4394
0.4383
0.4411
0.4379
0.4464
0.4434
0.4452
0.4450
0.4428
2.7
1.7
1.2
4.0
5.8
3.7
1.7
2.7
1.5
3.2
1.5
1.3
1.3
1.1
3.6
2.5
1.1
2.6
2.9
1.4
2.1
1.3
3.4
2.4
1.7
2.4
0.7
2.0
2.7
1.4
1.7
1.0
1.8
2.3
2.7
1.1
1.0
1.4
1.6
5.3
2.2
1.6
1.3
4.2
1.6
3.1
1.1
2.1
1.2
1.9
2.5
2.2
12MP40-35
12MP40-69
12MP40-73
12MP40-21
12MP40-25
12MP40-IC-139
12MP40-15
12MP40-IC-121
12MP40-49
12MP40-IC-131
12MP40-52
12MP40-9
12MP40-IC-147
12MP40-82
12MP40-IC-110
12MP40-26
12MP40-105
12MP40-34
12MP40-89
12MP40-95
12MP40-66
12MP40-75
12MP40-60
12MP40-IC-135
12MP40-56
12MP40-8
12MP40-47
12MP40-76
12MP40-65
12MP40-50
12MP40-54
12MP40-7
12MP40-IC-142
12MP40-90
12MP40-72
12MP40-12
12MP40-43
12MP40-45
12MP40-42
12MP40-13
12MP40-IC-118
12MP40-IC-138
12MP40-104
12MP40-93
12MP40-81
12MP40-100
12MP40-59
12MP40-24
12MP40-46
12MP40-IC-123
12MP40-97
12MP40-IC-117
248
113
436
163
185
141
399
260
270
237
224
352
162
365
150
174
406
155
265
95
163
491
56
143
252
282
84
231
223
302
213
341
205
294
135
229
84
247
243
136
388
81
161
166
293
120
84
125
189
104
88
160
128830
69664
565860
63184
255191
118044
152561
111438
143959
87297
139510
159940
36956
248956
128683
75045
342926
77195
148241
57373
51688
358956
69585
43685
31831
240803
44586
146814
131445
174800
153791
508583
72551
1661175
70656
189405
48099
129465
63681
180756
221991
39487
70254
153604
237081
79584
33955
70884
93743
49240
45705
93903
1.4
3.0
1.0
1.8
1.5
2.2
1.7
1.6
1.7
1.3
2.1
2.2
1.7
1.2
1.6
2.2
1.1
2.6
1.5
2.5
2.4
1.3
2.8
1.8
1.3
1.3
1.9
1.6
1.6
2.0
1.8
1.3
1.5
1.3
2.4
2.0
2.4
1.9
1.7
2.0
1.3
2.8
2.1
2.2
1.9
2.5
2.8
2.6
1.6
2.4
2.6
2.6
18.6301
18.6238
18.3706
18.5868
18.4860
18.3237
18.4100
18.4745
18.4552
18.3860
18.4649
18.6023
18.3774
18.4122
18.3988
18.6105
18.4646
18.5797
18.5650
18.5213
18.4202
18.4083
18.4871
18.5088
18.6934
18.6163
18.6575
18.5213
18.4946
18.5613
18.4516
18.5532
18.5299
18.5667
18.4483
18.5155
18.6981
18.5714
18.4972
18.4663
18.5733
18.4075
18.6233
18.6145
18.5306
18.7856
18.5184
18.6042
18.5385
18.4145
18.6167
18.3601
0.7
0.9
0.9
0.7
0.7
0.9
1.1
0.8
0.9
0.7
1.0
0.7
0.8
0.8
1.0
0.9
1.1
0.7
0.8
0.6
1.3
1.2
1.2
1.7
1.1
0.7
0.6
0.6
0.8
0.9
1.1
0.9
0.6
0.7
0.9
1.0
1.1
0.9
0.6
0.6
0.8
1.6
0.8
0.8
0.8
1.1
1.2
1.1
0.6
1.0
1.0
1.1
0.4395
0.4397
0.4458
0.4410
0.4435
0.4476
0.4455
0.4441
0.4454
0.4479
0.4460
0.4428
0.4486
0.4480
0.4483
0.4440
0.4483
0.4461
0.4468
0.4492
0.4520
0.4533
0.4515
0.4509
0.4471
0.4503
0.4494
0.4528
0.4535
0.4527
0.4554
0.4530
0.4536
0.4527
0.4556
0.4544
0.4505
0.4536
0.4555
0.4566
0.4543
0.4591
0.4543
0.4557
0.4584
0.4521
0.4591
0.4578
0.4599
0.4639
0.4592
0.4683
0.9
2.2
1.6
4.4
1.6
3.3
1.5
1.3
1.4
2.6
2.1
1.8
2.8
1.9
1.5
1.3
2.1
1.4
1.3
1.2
1.7
1.3
1.4
2.3
1.9
2.3
1.2
1.2
1.9
1.4
1.6
1.3
1.6
1.9
1.1
1.1
1.5
2.3
2.0
1.5
1.7
2.2
2.3
1.9
2.1
2.1
2.3
1.8
1.8
1.8
1.7
1.9
12MP40-58
12MP40-37
12MP40-94
12MP40-IC-116
12MP40-17
12MP40-IC-126
139
179
174
95
116
313
128381
166680
72254
19100
34477
440308
2.0
2.4
2.0
2.2
1.6
29.6
18.5901
18.3428
18.2258
17.8012
18.6696
12.9342
1.0
0.9
3.0
3.8
0.7
0.7
0.4631
0.4782
0.4824
0.5027
0.4795
2.0496
3.5
4.3
3.1
5.0
2.9
1.6
12MP41; Yukon-Tanana, Tracy Arm Assemblage, orthoquartzite, (Degree Decimal: 58.07589, 133.7
12MP41-18
331
8305
2.3 25.7111
13.4
0.0502
13.8
12MP41-56
245
10897
2.1 23.0073
14.6
0.0568
15.7
12MP41-88
191
12869
2.9 25.0753
30.4
0.0525
30.5
12MP41-36
214
7351
3.0 29.8463
48.6
0.0441
48.8
12MP41-57
381
18778
2.1 21.2073
7.0
0.0633
7.6
12MP41-51
158
6723
3.3 22.2625
28.7
0.0617
30.4
12MP41-77
238
12560
1.8 20.1541
12.0
0.1050
12.4
12MP41-87
254
113876
0.7 13.4641
0.7
1.7264
2.7
12MP41-68
94
80787
2.6 12.5992
1.8
1.8262
3.3
12MP41-96
31
35069
1.6 11.9366
5.0
2.6362
5.1
12MP41-1
93
128561
1.7 11.5853
1.3
2.7720
3.1
12MP41-95
91
107193
0.8
9.8427
0.9
3.8745
1.3
351
121725
5.0
9.7038
1.0
1.1187
4.3
12MP41-24
12MP41-100
323
353956
1.6
9.4022
0.4
4.2484
2.9
12MP41-60
30
50254
1.0
9.1106
1.4
4.9050
2.1
12MP41-30
29
32103
0.7
9.0901
1.0
4.8989
1.4
12MP41-97
90
136178
1.2
9.0502
0.6
4.8631
1.4
12MP41-37
25
17784
1.6
9.0335
2.3
3.9809
6.9
12MP41-61
26
32990
1.0
9.0060
2.8
4.7817
4.5
12MP41-19
127
162544
0.7
8.9607
0.7
4.8275
1.1
12MP41-64
40
52854
0.9
8.9507
2.1
5.0282
2.7
12MP41-27
52
42458
1.1
8.9480
1.4
5.0593
2.7
12MP41-54
55
91778
1.0
8.9440
1.1
4.9980
4.0
12MP41-12
57
44910
1.4
8.9275
0.8
4.9271
1.4
12MP41-99
145
180625
1.5
8.9268
0.5
4.5178
1.4
12MP41-6
49
58893
1.5
8.9100
1.4
4.8760
1.8
12MP41-59
31
44405
0.8
8.9064
3.2
4.4182
3.4
12MP41-49
44
225658
0.9
8.9032
2.2
4.9303
3.6
12MP41-91
129
124370
1.1
8.8916
0.5
4.8631
1.8
12MP41-16
74
58695
1.4
8.8753
0.8
4.9026
1.1
12MP41-67
23
61834
1.0
8.8719
2.4
5.1614
3.3
12MP41-76
61
108136
1.0
8.8718
0.7
5.0036
1.5
12MP41-66
59
56487
1.3
8.8713
1.0
5.0125
1.4
12MP41-44
83
130987
1.2
8.8710
0.9
5.1081
1.4
12MP41-29
28
27819
0.7
8.8652
2.6
5.0300
2.7
12MP41-93
36
42606
1.5
8.8611
1.2
5.1522
2.2
12MP41-81
45
44325
1.2
8.8605
1.8
5.0613
2.3
12MP41-84
35
51114
0.7
8.8577
1.9
5.1499
2.3
12MP41-32
57
90067
0.4
8.8545
1.2
5.1540
1.5
12MP41-79
16
36981
0.9
8.8511
2.2
5.1232
2.9
12MP41-94
61
94891
0.8
8.8505
1.2
4.9252
1.8
12MP41-75
83
83201
1.1
8.8475
0.8
4.8247
1.3
12MP41-40
40
42942
1.0
8.8330
2.1
4.9848
3.3
12MP41-62
111
135018
0.5
8.8294
0.4
5.1055
1.4
12MP41-14
12MP41-70
12MP41-90
12MP41-41
12MP41-15
12MP41-82
12MP41-78
12MP41-4
12MP41-34
12MP41-58
12MP41-33
12MP41-55
12MP41-52
12MP41-89
12MP41-11
12MP41-69
12MP41-7
12MP41-92
12MP41-47
12MP41-74
12MP41-50
12MP41-71
12MP41-46
12MP41-73
12MP41-98
12MP41-72
12MP41-53
12MP41-85
12MP41-23
12MP41-43
12MP41-13
12MP41-3
12MP41-48
12MP41-28
12MP41-21
12MP41-38
12MP41-39
12MP41-63
12MP41-31
12MP41-10
12MP41-45
12MP41-25
12MP41-26
12MP41-20
12MP41-5
1.
2.
3.
4.
48
69
38
68
25
41
16
22
47
50
74
77
22
29
25
207
36
32
37
45
75
37
62
119
49
25
46
25
65
56
35
51
30
47
67
49
103
44
45
33
44
30
25
38
35
39744
177209
45511
84015
75254
46664
19665
26148
74125
49774
76462
67520
19456
34615
28756
168910
48862
72583
64543
29507
62846
67421
78665
158242
49121
29522
48579
42943
134613
67203
38373
95228
59230
77456
83322
74297
189886
191154
145896
94159
62348
61936
75960
126677
61498
0.9
1.0
1.3
2.0
0.5
1.2
0.8
0.7
1.9
0.6
0.6
1.6
0.7
1.2
1.4
1.9
0.9
0.6
1.1
1.2
0.8
0.5
1.1
0.8
1.2
0.7
0.6
0.6
1.6
1.4
0.5
0.6
0.4
1.1
2.2
1.0
2.6
0.6
1.7
1.9
0.8
1.0
1.1
0.5
0.5
8.8174
8.8154
8.8129
8.8125
8.8067
8.7994
8.7879
8.7868
8.7036
8.6590
8.6377
8.6288
8.6003
8.5978
8.5690
8.5630
8.5547
8.5452
8.5334
8.5195
8.5143
8.5105
8.5021
8.4744
8.4727
8.4624
8.4404
8.4255
8.4217
7.8789
7.8707
7.8140
7.8011
7.7701
7.7645
6.7460
6.3087
5.9323
5.8087
5.7023
5.6052
5.4295
5.4027
5.3670
5.3382
1.4
1.0
1.4
0.9
2.4
1.6
2.4
2.7
1.0
1.5
0.7
0.9
2.3
2.5
1.2
0.4
1.5
1.3
1.5
1.9
1.1
2.2
1.1
0.5
1.3
2.6
0.8
1.8
0.8
0.8
1.3
1.1
1.3
0.8
0.5
1.0
2.0
1.0
0.6
0.8
0.5
1.0
0.6
0.6
0.7
4.9289
4.9971
5.3964
5.1193
5.1500
5.1558
5.1971
5.1902
5.1815
4.8586
5.0062
5.4274
5.5076
5.4615
5.5868
4.8462
5.5375
5.5320
5.5269
5.3206
5.4322
5.5725
4.9924
5.0286
5.3620
5.0590
5.5372
5.6275
5.3885
6.0108
6.5508
6.5245
6.3835
6.4941
6.2858
8.3277
9.5449
10.8322
11.1463
11.5401
10.9470
12.9292
13.2259
13.0686
13.5677
2.1
1.5
3.2
1.7
2.7
1.9
2.8
3.8
1.8
2.2
1.2
1.0
2.6
3.0
2.0
1.7
1.8
3.1
2.5
3.8
2.9
2.4
1.6
1.5
1.7
3.1
1.4
2.3
2.1
1.4
1.9
1.6
2.1
1.7
3.9
2.4
4.6
5.8
2.2
5.1
2.8
1.7
1.8
1.4
3.1
Analyses with >10% uncertainty (1-sigma) in 206Pb/238U age are not included.
Analyses with >10% uncertainty (1-sigma) in 206Pb/207Pb age are not included, unless 206Pb/238U
Best age is determined from 206Pb/238U age for analyses with 206Pb/238U age <900 Ma and from
Concordance is based on 206Pb/238U age / 206Pb/207Pb age. Value is not reported for 206Pb/23
5.
6.
7.
8.
9.
10.
11.
12.
13.
14.
15.
16.
17.
18
Analyses with 206Pb/238U age > 500 Ma and with >20% discordance (<80% concordance) are not
Analyses with 206Pb/238U age < 500 Ma, a manual discordance filter is applied and these analyses
(this is due to the strong metamorphic overprint from the nearby Coast Mountains Batholith as outlin
Analyses with 206Pb/238U age > 500 Ma and with >5% reverse discordance (<105% concordance)
All uncertainties are reported at the 1-sigma level, and include only measurement errors.
Systematic errors are as follows (at 2-sigma level): [Range= 0.7 to 1.1% (206Pb/238U) & 0.7-0.8% (
Analyses conducted by LA-MC-ICPMS, as described by Gehrels et al. (2008).
U concentration and U/Th are calibrated relative to Sri Lanka zircon standard and are accurate to ~2
Common Pb correction is from measured 204Pb with common Pb composition interpreted from Stac
Common Pb composition assigned uncertainties of 1.5 for 206Pb/204Pb, 0.3 for 207Pb/204Pb, and
U/Pb and 206Pb/207Pb fractionation is calibrated relative to fragments of a large Sri Lanka zircon of
U decay constants and composition as follows: 238U = 9.8485 x 10-10, 235U = 1.55125 x 10-10, 23
Weighted mean and concordia plots determined with Isoplot (Ludwig, 2008).
* designates age used in weighted mean and concordia plots per sample
Column "v" designates type of acquisition routine performed ( FAR= Faraday routine; IC = Ion Count
Gehrels, G.E., and Pecha, M., in review, Detrital Zircon U-Pb geochronology and Hf Isotope Geochemist
Gehrels, G.E., Valencia, V.A., Ruiz, J., 2008. Enhanced precision, accuracy, efficiency, and spatial resol
Ludwig, K.R., 2008, Isoplot 3.6: Berkeley Geochronology Center Special Publication No. 4, 77 p.
Stacey, J.S., and Kramers, J.D., 1975, Approximation of terrestrial lead isotopic evolution by a two-stage
Apparent ages (Ma)
206Pb*
238U
2, 131.25503)
0.0495
0.0551
0.0566
0.0575
0.0580
0.0581
0.0589
0.0595
0.0603
0.0608
0.0610
0.0612
0.0613
0.0616
0.0621
0.0623
0.0624
0.0624
0.0625
0.0625
0.0627
0.0627
0.0628
0.0630
0.0631
0.0631
0.0631
0.0632
0.0632
0.0632
0.0632
0.0633
0.0634
0.0634
0.0634
0.0634
0.0635
0.0637
0.0638
0.0638
0.0639
0.0639
0.0639
0.0639
0.0640
±
(%)
error
corr.
3.8
3.7
2.0
4.4
6.3
3.4
2.9
1.3
1.5
1.5
1.9
3.6
1.4
2.2
1.2
1.8
2.0
1.0
1.7
2.1
4.6
4.5
3.3
1.1
1.6
2.4
1.8
1.6
2.9
1.2
1.4
0.9
0.9
1.1
1.2
1.6
1.1
7.3
1.5
1.1
1.0
1.9
2.4
1.3
1.4
0.96
0.92
0.46
0.93
0.93
0.70
0.79
0.49
0.31
0.32
0.64
0.66
0.41
0.50
0.49
0.51
0.59
0.37
0.60
0.80
0.96
0.96
0.90
0.39
0.72
0.74
0.77
0.51
0.67
0.75
0.27
0.13
0.39
0.31
0.50
0.37
0.48
0.86
0.58
0.53
0.45
0.42
0.47
0.53
0.47
206Pb*
238U*
311.2
345.6
355.1
360.1
363.3
364.0
368.8
372.3
377.2
380.8
382.0
382.7
383.6
385.5
388.5
389.6
390.2
390.4
390.7
390.7
391.9
392.1
392.9
393.7
394.3
394.6
394.7
394.9
395.0
395.1
395.2
395.4
396.2
396.2
396.2
396.5
396.7
398.2
398.7
398.8
399.0
399.0
399.5
399.5
399.6
±
(Ma)
11.5
12.4
6.8
15.5
22.4
12.2
10.3
4.8
5.5
5.4
7.0
13.4
5.2
8.4
4.3
6.9
7.7
3.9
6.4
7.9
17.5
17.0
12.7
4.2
5.9
9.1
6.7
6.2
11.0
4.5
5.3
3.6
3.4
4.4
4.5
6.3
4.4
28.1
5.7
4.2
3.7
7.3
9.1
5.0
5.6
207Pb*
235U
325.8
352.5
353.7
371.4
370.2
372.3
377.9
373.7
384.6
376.2
391.0
393.3
391.8
403.2
391.4
386.8
395.3
395.7
394.5
397.0
394.8
396.6
397.9
392.5
398.3
401.1
401.9
398.6
401.1
399.2
408.1
400.4
399.6
404.6
403.0
413.0
400.0
395.8
403.6
401.5
405.6
425.5
401.0
408.9
410.4
±
(Ma)
11.0
12.0
12.8
14.7
21.2
15.3
11.5
8.4
15.5
14.3
9.5
17.7
11.1
15.0
7.6
11.7
11.3
9.3
9.2
8.6
15.6
15.3
12.1
9.0
7.1
10.6
7.5
10.4
14.3
5.1
17.6
23.9
7.6
12.2
7.9
15.0
7.9
27.6
8.5
6.9
7.1
15.7
16.5
8.2
10.4
206Pb*
207Pb*
431.4
398.2
345.1
442.1
413.0
424.5
434.4
382.5
429.5
347.8
444.8
456.2
440.8
505.9
408.5
370.2
425.1
426.8
416.7
434.0
411.8
422.6
427.0
385.3
421.7
438.6
443.9
419.9
436.5
422.8
481.9
429.2
419.1
452.8
442.0
506.6
418.6
381.4
432.2
417.1
443.2
571.5
409.7
461.9
471.6
±
(Ma)
25.3
36.4
86.2
37.6
57.1
77.6
49.9
52.7
102.9
97.8
50.2
90.2
69.1
86.3
45.3
70.4
62.6
58.7
49.8
35.3
28.3
30.9
35.8
57.3
33.7
47.6
32.1
60.7
71.8
22.7
111.5
159.9
47.3
77.4
45.8
90.6
47.0
95.6
46.4
39.5
42.1
89.4
98.0
45.6
59.8
0.0640
0.0640
0.0641
0.0642
0.0642
0.0643
0.0643
0.0643
0.0643
0.0644
0.0644
0.0645
0.0645
0.0645
0.0645
0.0645
0.0646
0.0646
0.0647
0.0647
0.0648
0.0648
0.0648
0.0649
0.0649
0.0649
0.0649
0.0650
0.0650
0.0650
0.0650
0.0650
0.0650
0.0650
0.0651
0.0651
0.0651
0.0652
0.0652
0.0654
0.0654
0.0655
0.0656
0.0657
0.0658
0.0658
0.0661
0.0661
0.0661
0.0663
0.0663
0.0664
0.7
1.5
0.9
0.8
0.9
0.5
1.5
3.7
1.5
0.9
1.2
0.9
2.0
0.6
1.3
1.5
1.2
1.4
3.7
0.9
4.0
1.8
2.6
1.2
2.1
1.4
1.3
1.4
1.3
0.9
2.1
1.0
0.9
1.1
2.3
0.5
0.7
1.5
1.0
2.1
3.5
1.8
0.7
0.9
0.8
0.9
1.2
1.3
0.9
3.2
1.5
1.9
0.21
0.42
0.51
0.61
0.29
0.28
0.57
0.95
0.49
0.17
0.58
0.48
0.64
0.25
0.58
0.71
0.42
0.50
0.86
0.17
0.69
0.51
0.74
0.40
0.21
0.53
0.75
0.66
0.30
0.22
0.58
0.39
0.35
0.28
0.93
0.28
0.34
0.55
0.38
0.62
0.87
0.87
0.24
0.37
0.40
0.30
0.68
0.22
0.24
0.83
0.46
0.40
400.0
400.1
400.2
401.1
401.3
401.4
401.4
401.7
401.8
402.5
402.6
402.8
402.8
402.9
403.0
403.1
403.5
403.6
404.0
404.3
404.6
404.7
404.8
405.1
405.4
405.6
405.6
405.8
405.8
406.0
406.0
406.0
406.2
406.2
406.3
406.5
406.7
407.2
407.3
408.2
408.5
409.3
409.5
410.0
410.8
410.9
412.4
412.6
412.7
413.6
413.6
414.5
2.8
5.6
3.3
3.2
3.4
2.0
5.9
14.4
5.8
3.7
4.6
3.6
8.0
2.5
5.1
6.0
4.6
5.5
14.4
3.3
15.5
7.1
10.1
4.9
8.4
5.4
5.2
5.5
5.0
3.5
8.4
4.0
3.4
4.2
9.2
2.0
2.6
5.7
4.1
8.1
13.7
7.0
2.6
3.5
3.0
3.7
4.7
5.2
3.6
12.7
6.1
7.5
400.0
398.1
400.7
403.2
403.7
404.5
402.5
399.4
407.7
409.8
401.2
405.9
398.2
409.4
414.5
408.3
402.3
400.7
405.4
406.2
418.4
400.4
411.1
409.2
423.2
410.9
405.8
406.1
402.1
402.4
409.7
411.1
403.3
417.3
406.3
406.6
406.7
406.8
407.9
416.3
409.7
405.7
410.6
403.3
407.8
405.8
418.2
406.5
411.9
419.5
415.6
425.1
11.0
11.3
5.6
4.4
10.0
6.2
8.9
12.9
10.2
18.2
6.7
6.5
10.6
8.8
7.6
7.3
9.3
9.2
14.2
16.6
19.6
11.8
11.8
10.5
34.9
8.7
6.0
7.1
14.0
13.5
12.5
8.8
8.1
13.0
8.4
5.9
6.6
8.9
9.2
11.3
13.5
6.7
9.3
8.0
6.3
10.3
5.8
19.6
12.4
13.2
11.3
16.2
400.2
386.4
403.4
415.4
417.8
421.8
408.4
386.2
441.3
451.1
393.5
423.8
371.2
446.2
478.7
437.9
395.4
384.0
413.6
416.9
494.7
375.5
446.8
432.5
521.1
441.1
406.8
408.3
380.6
382.0
430.5
439.4
386.8
479.1
406.6
407.0
406.7
404.7
411.1
461.4
416.5
385.3
416.7
365.3
390.9
377.3
450.1
371.8
407.8
452.0
426.5
482.8
73.1
69.8
32.4
23.6
64.4
40.0
49.0
28.2
58.7
117.9
37.3
38.1
55.5
56.4
40.0
34.1
57.0
54.2
48.0
109.0
91.1
69.5
52.6
63.8
216.5
49.0
26.5
35.7
90.2
89.5
67.8
53.5
51.0
80.9
20.8
37.7
41.3
49.8
57.0
57.1
44.0
21.9
59.5
50.0
38.4
65.9
27.6
128.5
79.3
48.0
66.0
94.5
0.0664
0.0666
0.0666
0.0677
0.0682
0.0710
0.8
1.8
2.0
5.9
5.7
0.8
0.26
0.41
0.42
0.84
0.66
0.21
414.6
415.6
415.7
422.5
425.5
442.2
3.3
7.2
8.1
24.2
23.5
3.4
410.6
418.7
406.5
436.1
420.8
442.6
10.7
15.3
16.3
25.1
29.6
13.3
388.3
435.7
354.9
508.6
394.9
444.6
68.7
90.5
99.8
85.4
144.5
80.9
131.25776)
0.0436
0.0513
0.0541
0.0545
0.0556
0.0567
0.0584
0.0585
0.0586
0.0588
0.0589
0.0591
0.0592
0.0592
0.0592
0.0593
0.0594
0.0594
0.0594
0.0594
0.0595
0.0595
0.0596
0.0596
0.0596
0.0597
0.0597
0.0597
0.0597
0.0599
0.0599
0.0599
0.0600
0.0600
0.0601
0.0601
0.0601
0.0602
0.0602
0.0603
0.0603
0.0603
0.0603
0.0603
1.2
4.7
9.7
1.8
4.5
0.9
5.0
1.8
1.7
2.4
1.4
2.0
1.9
5.4
4.2
0.9
2.1
2.1
2.7
1.7
3.6
1.6
1.9
2.9
1.9
0.7
1.2
1.6
1.1
0.7
2.1
1.6
1.3
0.7
2.7
1.3
2.8
2.7
1.8
1.5
0.8
1.4
2.3
1.9
0.91
0.98
1.00
0.98
0.40
0.81
0.83
0.52
0.19
0.58
0.29
0.25
0.35
0.55
0.74
0.24
0.26
0.46
0.38
0.16
0.51
0.39
0.36
0.36
0.39
0.20
0.87
0.49
0.18
0.74
0.65
0.24
0.17
0.16
0.38
0.60
0.53
0.16
0.31
0.36
0.38
0.23
0.39
0.74
275.4
322.3
339.5
341.9
348.6
355.4
365.8
366.4
367.2
368.6
368.8
370.1
370.6
370.7
371.0
371.3
371.8
372.0
372.2
372.2
372.6
372.8
373.2
373.3
373.4
373.7
373.7
373.7
373.8
374.8
374.9
375.0
375.4
375.9
376.2
376.3
376.4
376.7
377.1
377.3
377.4
377.6
377.6
377.7
3.2
14.9
32.2
6.0
15.3
3.2
17.6
6.4
5.9
8.4
5.0
7.2
6.8
19.5
15.1
3.3
7.5
7.7
9.9
6.1
13.0
5.8
6.7
10.6
7.0
2.7
4.4
5.8
4.0
2.5
7.7
5.7
4.6
2.4
10.0
4.8
10.3
9.7
6.6
5.5
2.8
5.2
8.3
6.9
285.8
333.1
346.8
346.1
358.2
360.5
367.9
368.5
360.1
376.8
378.1
353.3
353.3
379.4
385.2
376.5
386.1
380.1
366.9
362.6
366.9
372.2
362.4
378.6
363.2
376.4
379.1
376.2
389.7
377.9
372.2
363.8
370.2
370.5
358.6
375.9
387.5
391.3
373.1
387.3
377.2
369.7
370.8
377.3
3.2
13.7
28.6
5.4
33.8
3.4
18.4
10.8
25.9
12.8
15.2
24.1
16.2
31.1
18.1
12.2
26.1
14.6
22.2
32.6
21.5
12.7
15.9
25.9
15.3
11.5
4.4
10.2
19.5
3.0
10.1
20.0
22.5
12.8
21.9
6.9
17.0
54.2
17.8
13.5
6.3
18.8
17.9
8.0
372.1
408.9
395.8
374.4
420.7
393.1
381.3
381.7
315.3
427.9
435.4
244.6
241.1
432.4
471.2
408.6
472.5
430.0
333.8
301.2
331.1
368.5
293.7
411.4
298.6
393.4
412.1
391.5
484.9
397.0
355.8
293.0
337.9
336.6
246.3
373.7
454.7
478.8
348.2
446.9
376.4
320.7
328.6
375.3
11.8
22.1
14.6
8.1
229.0
14.9
74.9
67.0
190.6
73.6
102.8
180.2
117.8
182.7
83.7
84.5
173.8
90.9
151.0
241.6
135.6
84.7
111.0
171.7
105.4
80.5
15.2
63.5
131.1
14.3
55.2
145.4
162.1
92.4
154.8
39.4
99.2
365.8
122.4
87.2
41.3
134.3
120.0
38.2
0.0603
0.0603
0.0604
0.0604
0.0604
0.0604
0.0604
0.0604
0.0605
0.0605
0.0606
0.0606
0.0606
0.0606
0.0606
0.0607
0.0607
0.0607
0.0608
0.0608
0.0608
0.0608
0.0609
0.0609
0.0609
0.0609
0.0610
0.0610
0.0610
0.0610
0.0611
0.0611
0.0611
0.0612
0.0612
0.0612
0.0613
0.0614
0.0614
0.0614
0.0614
0.0615
0.0615
0.0615
0.0616
0.0617
0.0617
0.0618
0.0618
0.0619
0.0621
0.0622
1.0
1.0
1.5
2.1
2.5
1.4
3.5
2.4
2.7
0.7
2.0
1.3
1.9
2.8
1.2
1.8
1.3
1.1
2.1
1.3
0.9
1.6
3.0
1.0
1.1
1.3
3.8
2.9
1.4
1.8
1.7
2.5
1.3
1.9
1.2
0.9
1.1
1.1
1.0
3.0
0.6
1.4
3.2
1.5
1.4
4.2
1.1
1.5
2.5
1.3
1.1
4.7
0.71
0.86
0.22
0.95
0.97
0.19
0.53
0.94
0.45
0.48
0.35
0.54
0.39
0.52
0.85
0.92
0.81
0.31
0.29
0.67
0.65
0.22
0.48
0.74
0.89
0.25
0.88
0.25
0.76
0.42
0.82
0.25
0.83
0.94
0.29
0.78
0.86
0.90
0.54
0.42
0.41
0.69
0.97
0.92
0.44
0.51
0.72
0.65
0.42
0.78
0.80
0.38
377.7
377.7
377.8
377.9
378.0
378.0
378.3
378.3
378.6
378.9
379.0
379.1
379.2
379.2
379.3
379.6
379.7
380.2
380.2
380.3
380.5
380.7
381.0
381.0
381.1
381.2
381.4
381.4
381.8
382.0
382.0
382.1
382.6
382.7
382.9
383.1
383.7
384.0
384.0
384.2
384.4
384.5
384.7
385.0
385.6
385.8
386.0
386.4
386.5
387.4
388.5
389.1
3.5
3.5
5.4
7.6
9.3
5.2
12.8
8.6
9.9
2.6
7.3
4.6
7.0
10.2
4.6
6.7
4.9
4.1
7.9
4.8
3.3
6.1
11.1
3.6
4.0
4.9
14.2
10.7
5.1
6.6
6.3
9.2
4.8
7.0
4.3
3.3
4.1
4.0
3.7
11.1
2.3
5.3
12.0
5.6
5.3
15.9
4.0
5.8
9.5
4.8
4.2
17.7
379.9
380.4
388.0
380.7
377.0
381.2
384.6
383.5
380.6
381.2
390.5
382.5
380.6
381.2
380.9
380.0
382.3
375.5
358.4
382.2
381.9
393.2
368.1
384.5
382.9
378.6
379.7
358.0
382.6
378.2
385.9
379.3
382.6
383.3
386.6
385.3
385.5
385.1
385.3
393.3
389.1
384.9
385.9
384.9
385.9
388.2
387.2
387.3
389.7
390.2
389.7
376.8
4.3
3.6
21.9
6.9
8.2
24.2
21.2
7.9
19.1
4.7
18.3
7.5
15.5
16.9
4.6
6.3
5.2
11.4
22.2
6.2
4.4
24.8
19.2
4.2
3.9
16.9
13.8
34.5
5.8
13.5
6.7
31.6
4.9
6.4
12.9
3.6
4.1
3.8
5.9
23.0
4.8
6.6
10.6
5.2
10.2
26.7
4.7
7.6
19.4
5.3
4.5
38.5
393.6
396.8
449.4
397.4
371.4
400.9
422.5
414.6
393.0
395.7
458.9
402.7
389.7
393.6
390.9
382.3
398.0
346.7
219.6
394.0
390.8
467.8
287.9
405.5
393.6
363.0
369.4
209.1
387.3
355.3
409.0
362.2
383.0
387.0
408.9
398.1
396.0
392.2
393.4
447.4
417.2
386.7
393.2
384.3
388.2
403.1
394.3
392.7
408.5
407.0
396.6
301.9
21.5
13.0
147.6
14.9
15.1
167.9
125.4
18.2
120.6
28.9
117.4
44.5
101.0
101.6
17.0
17.5
21.8
78.1
162.8
32.7
23.3
164.4
125.1
19.7
12.6
117.2
46.5
257.4
26.8
87.8
26.8
218.6
19.4
15.3
86.2
15.9
14.8
11.5
34.6
142.4
30.4
33.3
16.8
14.4
63.9
159.4
22.6
40.5
122.1
22.9
18.6
257.7
0.0624
0.0624
0.0627
1.9
4.2
2.5
0.22
0.94
0.37
389.9
390.1
392.1
7.2
16.1
9.6
384.9
389.3
386.4
27.2
14.6
21.7
355.0
384.7
352.4
187.0
34.6
141.8
31.23030)
0.0458
0.0481
0.0501
0.0517
0.0519
0.0522
0.0528
0.0532
0.0549
0.0553
0.0558
0.0563
0.0563
0.0564
0.0564
0.0568
0.0569
0.0570
0.0570
0.0574
0.0575
0.0578
0.0578
0.0580
0.0582
0.0583
0.0583
0.0584
0.0584
0.0584
0.0585
0.0585
0.0586
0.0586
0.0586
0.0587
0.0587
0.0587
0.0588
0.0588
0.0588
0.0588
0.0589
0.0589
0.0589
0.0590
0.0590
1.4
4.4
2.9
5.1
6.4
4.1
3.1
4.2
2.7
1.0
1.5
2.2
3.1
1.3
1.8
1.0
5.2
6.3
2.2
1.2
1.5
1.9
3.1
1.0
0.7
3.1
0.9
0.9
2.5
1.5
1.1
1.2
6.3
1.6
1.3
0.7
0.7
0.8
1.1
1.5
2.0
3.6
2.0
1.3
0.8
2.5
0.9
0.79
0.88
0.93
0.80
0.96
0.82
0.69
0.93
0.70
0.44
0.36
0.64
0.75
0.43
0.64
0.49
0.76
0.78
0.58
0.25
0.61
0.24
0.76
0.27
0.40
0.62
0.29
0.18
0.94
0.66
0.49
0.49
0.89
0.43
0.21
0.28
0.48
0.27
0.30
0.63
0.79
0.45
0.83
0.24
0.21
0.64
0.40
288.4
302.9
315.1
325.0
326.2
328.2
331.6
334.4
344.6
347.3
350.2
352.8
353.3
353.4
353.9
356.4
356.7
357.1
357.4
359.6
360.7
362.1
362.1
363.2
364.9
365.4
365.5
365.8
366.0
366.1
366.3
366.5
366.8
367.3
367.4
367.6
367.9
367.9
368.1
368.3
368.4
368.5
368.8
368.9
369.0
369.3
369.5
3.8
13.2
8.9
16.3
20.3
13.1
10.1
13.7
9.1
3.3
5.2
7.7
10.5
4.5
6.0
3.4
18.0
21.8
7.5
4.1
5.4
6.6
10.9
3.6
2.3
10.9
3.3
3.2
8.8
5.5
3.8
4.2
22.6
5.6
4.7
2.6
2.4
2.8
3.9
5.4
7.1
13.0
7.3
4.7
2.9
9.0
3.3
296.0
310.3
317.8
331.4
330.5
331.6
338.0
337.8
349.5
351.1
360.3
356.7
352.1
354.5
360.9
360.9
363.2
371.7
360.3
355.3
365.5
351.5
360.0
367.8
367.1
364.5
366.1
368.1
367.7
371.0
368.1
362.4
368.7
368.5
387.1
368.4
368.6
369.0
355.1
372.0
368.8
378.9
375.1
364.4
368.5
381.8
370.4
4.4
13.6
8.5
18.2
18.7
14.2
13.1
12.9
11.5
6.6
12.8
10.5
12.0
9.1
8.3
6.0
20.9
25.0
11.4
13.8
7.6
22.9
12.3
11.6
5.1
15.3
9.9
15.3
8.2
7.3
6.7
7.4
22.2
11.5
20.1
8.1
4.3
9.0
11.0
7.4
7.8
25.8
7.7
16.7
11.9
12.5
7.2
356.0
366.7
337.9
376.3
360.7
355.0
381.8
361.5
382.5
376.1
426.0
382.1
344.5
361.9
406.5
389.9
405.1
463.5
379.6
327.7
396.0
282.0
346.4
396.8
380.6
358.8
370.0
382.7
378.5
401.4
379.7
336.0
380.3
376.0
506.7
373.4
372.9
375.8
270.6
395.0
371.8
442.9
413.9
335.7
365.1
458.7
376.3
23.4
54.8
25.9
86.5
39.9
64.9
74.4
37.2
62.9
44.9
87.3
59.7
60.2
62.0
47.2
38.8
100.0
110.7
69.4
101.3
44.0
171.3
59.4
81.4
34.3
88.8
69.8
109.4
21.1
39.8
42.8
48.1
74.9
75.6
134.4
56.5
27.3
63.3
80.2
41.6
35.0
162.4
31.0
120.1
84.8
67.3
47.8
0.0590
0.0590
0.0590
0.0591
0.0591
0.0591
0.0592
0.0592
0.0593
0.0593
0.0593
0.0593
0.0593
0.0594
0.0594
0.0594
0.0594
0.0595
0.0595
0.0595
0.0596
0.0596
0.0596
0.0596
0.0596
0.0596
0.0597
0.0597
0.0597
0.0597
0.0597
0.0598
0.0598
0.0598
0.0599
0.0599
0.0599
0.0599
0.0600
0.0601
0.0603
0.0603
0.0604
0.0605
0.0605
0.0605
0.0606
0.0608
0.0612
0.0614
0.0615
0.0616
2.6
1.7
1.1
1.0
0.8
1.3
2.1
1.2
1.6
0.8
1.3
0.7
2.1
2.2
1.1
1.7
0.9
0.9
1.6
2.0
1.4
2.6
0.8
1.3
1.0
1.2
1.7
0.9
1.5
0.7
1.3
2.0
1.7
1.0
1.6
2.1
2.7
0.9
3.3
1.5
1.1
0.6
1.3
1.6
1.2
1.5
1.9
2.9
1.9
1.0
1.0
0.9
0.78
0.48
0.33
0.32
0.19
0.73
0.48
0.33
0.48
0.24
0.40
0.24
0.36
0.27
0.28
0.60
0.29
0.50
0.73
0.48
0.25
0.59
0.43
0.36
0.27
0.28
0.46
0.31
0.51
0.20
0.36
0.48
0.23
0.33
0.45
0.40
0.66
0.27
0.27
0.36
0.18
0.23
0.65
0.23
0.25
0.45
0.46
0.57
0.41
0.27
0.57
0.29
369.5
369.7
369.8
370.1
370.3
370.3
370.5
371.0
371.1
371.2
371.6
371.6
371.6
371.7
371.8
372.1
372.3
372.5
372.5
372.7
372.9
373.0
373.1
373.2
373.2
373.5
373.7
373.8
373.8
373.9
374.0
374.2
374.4
374.6
374.8
375.0
375.1
375.3
375.6
376.4
377.3
377.6
378.2
378.4
378.6
378.6
379.1
380.5
382.6
384.3
384.6
385.2
9.5
6.1
3.8
3.4
3.0
4.8
7.7
4.4
5.8
2.8
4.8
2.4
7.7
8.0
3.9
6.2
3.2
3.2
5.9
7.1
5.2
9.4
2.8
4.6
3.7
4.4
6.2
3.2
5.4
2.5
4.7
7.3
6.0
3.7
5.8
7.7
9.7
3.3
12.2
5.3
3.8
2.2
4.7
6.0
4.4
5.4
7.0
10.9
7.2
3.6
3.9
3.3
371.0
370.9
365.9
374.2
377.3
371.9
374.0
371.3
358.1
367.1
371.1
371.7
375.7
370.8
371.9
371.3
371.0
377.7
374.6
375.5
362.8
383.7
379.2
383.5
375.7
368.5
374.4
369.5
374.1
372.8
370.0
380.1
385.2
371.5
379.5
378.8
376.5
381.5
358.5
375.3
383.5
377.9
380.5
383.1
385.7
374.1
382.0
384.6
382.9
375.6
389.2
383.4
10.5
10.9
9.9
9.3
13.9
5.8
14.0
11.8
10.2
9.8
10.4
8.7
18.8
25.4
11.9
8.9
9.5
5.6
7.0
12.8
17.1
13.9
5.7
11.2
11.8
13.4
11.7
8.8
9.1
10.5
11.0
13.4
23.4
9.4
11.3
16.6
12.7
10.8
37.9
12.7
18.4
8.3
6.2
22.1
15.3
10.1
13.3
16.5
15.2
11.4
5.8
9.6
380.0
378.6
341.2
400.2
420.4
382.1
395.8
372.9
274.4
341.4
368.5
372.3
401.4
365.5
372.5
366.2
363.1
409.3
387.2
393.2
299.0
448.3
416.6
445.8
391.0
337.2
378.5
342.3
375.8
366.4
345.4
416.2
450.2
352.2
408.1
402.1
384.7
419.6
248.8
368.4
421.3
379.7
394.7
411.9
428.3
346.1
399.8
409.2
384.8
322.5
416.8
372.8
47.3
68.8
68.9
62.7
96.5
28.5
88.4
80.6
67.9
69.6
69.5
61.1
125.5
177.3
82.5
51.9
65.8
34.6
34.5
80.3
124.1
77.9
36.2
72.8
81.2
94.4
74.8
61.1
56.1
74.2
74.9
82.7
157.8
64.3
71.4
107.4
68.2
72.8
279.4
85.1
126.2
57.8
33.3
150.4
102.7
65.4
83.2
94.9
98.0
79.9
33.0
64.4
0.0637
0.0645
0.0660
1.8
7.2
1.5
0.35
0.73
0.25
397.9
402.8
412.0
6.9
28.3
5.9
397.4
414.2
407.8
16.8
34.0
19.9
394.3
478.0
384.0
107.4
152.0
129.3
0.0145
0.0147
0.0428
0.0586
0.0597
0.0653
0.0669
0.0678
0.0686
0.0687
0.0692
0.0699
0.0699
0.0702
0.0710
0.0710
0.0711
0.0713
0.0713
0.0717
0.0717
0.0729
0.0737
0.0775
0.0775
0.0780
1.9
1.1
4.8
4.9
4.8
0.9
3.7
1.6
1.4
2.5
1.1
2.4
4.6
1.1
2.7
1.6
3.8
0.6
1.7
1.4
1.9
0.7
2.9
2.5
6.4
4.2
0.67
0.28
0.99
0.99
0.98
0.71
0.98
0.93
0.91
0.36
0.89
0.94
0.97
0.86
0.94
0.86
0.95
0.46
0.85
0.85
0.93
0.66
0.90
0.96
0.95
0.99
93.0
94.3
270.3
367.4
373.9
408.1
417.5
422.9
428.0
428.3
431.6
435.6
435.8
437.5
442.0
442.1
442.7
444.0
444.2
446.4
446.6
453.8
458.3
480.9
481.1
484.2 *
1.7
1.0
12.7
17.7
17.4
3.8
14.8
6.4
5.7
10.3
4.6
10.0
19.5
4.8
11.3
6.9
16.2
2.7
7.3
6.2
8.2
3.3
12.6
11.7
29.5
95.2
97.8
289.5
375.1
382.3
411.6
420.4
429.4
431.4
438.0
432.7
435.3
437.1
439.0
440.1
444.9
441.4
444.2
442.8
446.0
448.8
459.7
458.5
475.5
477.3
475.9
2.5
3.5
12.2
15.7
15.5
4.6
12.8
5.9
5.3
24.4
4.3
8.9
16.9
4.7
10.1
6.7
14.3
4.9
7.2
6.1
7.4
4.2
11.7
9.9
25.7
16.2
151.7
185.8
447.8
423.0
433.3
431.7
436.3
464.8
449.5
489.7
438.6
433.4
444.0
446.6
429.8
459.4
434.3
445.2
435.7
443.9
460.1
489.0
459.1
449.6
458.8
435.6
47.7
83.9
14.5
18.4
19.2
21.2
15.3
14.0
13.9
141.0
12.7
18.5
23.8
15.1
21.1
20.7
29.0
27.1
23.6
19.8
16.7
18.9
30.4
15.6
48.5
15.7
042, 131.32230)
0.0569
0.0604
0.0612
0.0622
0.0638
0.0649
0.0658
0.0658
0.0661
0.0661
0.0662
0.0664
0.0665
0.0665
0.0665
0.0665
0.0666
0.0666
0.0668
5.6
2.2
2.2
5.0
3.4
7.7
1.9
1.4
1.4
4.6
2.4
2.2
3.0
1.7
1.3
1.3
1.3
1.9
1.7
0.63
0.91
0.88
0.96
0.98
0.99
0.39
0.72
0.64
0.97
0.55
0.50
0.37
0.33
0.21
0.28
0.26
0.19
0.22
356.5
377.8
382.9
388.9
398.8
405.6
410.5
410.6
412.3
412.6
413.3
414.3
414.9
415.1
415.2
415.2
415.6
415.7
416.6
19.5
8.0
8.3
19.0
13.2
30.1
7.6
5.7
5.6
18.4
9.6
8.7
12.1
6.7
5.2
5.1
5.3
7.5
6.9
364.9
384.9
391.8
390.9
404.1
411.1
416.2
417.3
418.7
419.9
408.7
415.5
408.9
423.0
420.2
422.5
414.1
445.8
409.9
27.2
7.7
8.3
17.1
11.7
26.1
16.9
6.8
7.5
16.3
14.7
14.7
27.5
17.5
20.9
15.7
17.2
35.5
25.6
418.6
428.0
444.5
402.8
434.5
442.0
447.6
454.1
454.2
460.4
382.4
422.3
374.8
465.9
447.9
462.6
406.3
604.1
372.1
153.4
22.7
27.4
33.8
16.4
23.5
101.7
30.6
37.4
24.6
81.8
83.2
171.3
106.0
131.9
96.9
109.4
209.7
166.6
0.0668
0.0670
0.0670
0.0671
0.0672
0.0672
0.0672
0.0672
0.0672
0.0673
0.0673
0.0674
0.0675
0.0675
0.0676
0.0676
0.0676
0.0676
0.0677
0.0677
0.0677
0.0678
0.0678
0.0678
0.0678
0.0678
0.0678
0.0678
0.0679
0.0679
0.0680
0.0680
0.0681
0.0681
0.0681
0.0681
0.0682
0.0682
0.0683
0.0683
0.0683
0.0683
0.0683
0.0684
0.0684
0.0684
0.0684
0.0685
0.0685
0.0685
0.0685
0.0685
1.7
1.3
1.5
1.7
1.3
1.0
2.6
1.4
2.4
0.8
1.9
1.6
1.5
1.8
1.4
1.3
3.1
0.8
4.2
1.3
1.4
1.5
1.9
1.8
1.6
2.0
1.5
2.1
0.9
1.6
1.7
3.5
3.0
1.6
2.2
2.0
1.3
1.4
3.6
1.2
1.1
2.0
1.4
1.0
2.2
1.7
4.4
0.7
1.0
2.1
2.1
1.1
0.37
0.20
0.46
0.60
0.29
0.66
0.80
0.52
0.60
0.61
0.63
0.27
0.76
0.41
0.45
0.56
0.88
0.42
0.92
0.88
0.28
0.27
0.45
0.64
0.75
0.37
0.62
0.69
0.19
0.41
0.58
0.76
0.54
0.68
0.44
0.64
0.63
0.30
0.90
0.89
0.37
0.66
0.29
0.41
0.66
0.66
0.85
0.46
0.70
0.78
0.77
0.41
416.8
418.0
418.0
418.7
419.0
419.1
419.2
419.3
419.4
419.7
420.0
420.4
420.9
421.3
421.5
421.9
421.9
422.0
422.1
422.3
422.3
422.7
422.8
422.9
423.0
423.0
423.0
423.2
423.5
423.5
423.9
423.9
424.4
424.6
424.9
424.9
425.1
425.3
425.8
425.9
425.9
426.0
426.1
426.5
426.5
426.5
426.6
426.8
426.9
426.9
426.9
427.0
7.0
5.1
6.1
7.0
5.2
4.1
10.5
5.7
9.9
3.4
7.6
6.4
6.3
7.5
5.6
5.3
12.8
3.2
17.4
5.4
5.8
6.0
7.8
7.5
6.6
8.4
6.0
8.5
3.6
6.4
6.9
14.3
12.1
6.5
9.0
8.1
5.4
6.0
14.6
4.8
4.7
8.3
5.7
4.3
8.9
7.0
18.3
2.9
4.2
8.7
8.5
4.7
413.4
417.5
420.2
422.0
420.8
421.0
422.4
424.0
424.2
426.6
419.3
431.6
420.7
434.1
425.2
424.7
422.7
422.3
416.5
424.7
433.1
431.7
423.7
427.3
425.9
417.2
421.4
421.0
425.7
424.6
431.9
423.6
419.8
422.4
412.9
429.6
427.8
428.4
425.4
426.3
427.7
427.5
434.1
425.0
428.7
430.7
429.5
429.5
427.3
421.0
428.5
434.8
15.8
21.5
11.3
9.9
15.4
5.3
11.3
9.3
14.0
4.8
10.1
20.6
7.0
15.8
10.6
8.1
12.3
6.4
15.8
5.2
17.7
19.0
14.6
10.0
7.4
18.9
8.1
10.3
16.6
13.2
10.2
15.9
18.7
8.1
16.9
10.8
7.2
16.9
13.7
4.5
10.8
10.6
16.9
9.0
11.4
9.0
18.2
5.4
5.1
9.4
9.3
9.9
394.2
415.0
432.5
440.2
430.8
431.6
439.9
449.6
450.2
464.4
415.5
491.8
419.8
502.7
445.2
439.9
426.8
424.3
385.4
438.1
490.9
480.0
428.3
451.1
441.9
385.2
412.8
409.1
437.7
430.2
474.8
422.0
394.3
410.5
346.0
455.0
442.1
445.1
423.0
428.5
437.8
435.3
476.7
417.1
440.6
452.8
445.0
443.9
429.7
388.6
436.9
476.4
97.2
137.8
64.8
51.1
95.6
25.9
43.9
51.1
71.4
24.1
51.1
124.5
29.3
89.8
60.5
43.2
38.1
37.4
40.3
15.9
106.6
114.8
83.8
49.0
31.4
115.5
40.9
48.1
104.5
77.4
51.9
66.7
102.3
38.4
101.1
52.8
35.8
102.3
38.0
13.0
64.0
50.5
101.3
52.7
54.7
42.4
59.9
30.4
23.0
38.7
37.5
56.7
0.0687
0.0687
0.0688
0.0688
0.0689
0.0689
0.0689
0.0689
0.0689
0.0690
0.0690
0.0690
0.0691
0.0692
0.0692
0.0695
0.0696
0.0697
0.0697
0.0707
0.0709
0.0714
0.0726
3.2
3.1
2.2
1.6
2.2
2.2
1.4
1.3
1.2
0.9
2.0
1.4
3.0
5.7
2.2
2.0
0.8
3.7
1.9
2.5
5.2
9.3
2.5
0.71
0.67
0.51
0.81
0.76
0.72
0.69
0.30
0.33
0.77
0.30
0.37
0.87
0.97
0.68
0.42
0.39
0.82
0.62
0.83
0.47
0.99
0.62
428.5
428.5
429.0
429.2
429.3
429.4
429.5
429.7
429.8
429.8
429.9
430.0
430.9
431.2
431.3
433.3
433.5
434.2
434.6
440.4
441.4
444.8
451.6
13.4
13.0
9.2
6.6
9.2
9.0
5.7
5.4
5.0
3.8
8.2
5.9
12.6
23.7
9.1
8.4
3.3
15.4
8.1
10.8
22.1
40.1
11.1
431.5
428.4
428.0
430.3
430.7
432.6
431.8
430.7
425.6
431.2
438.2
427.3
431.0
432.9
430.2
440.3
431.5
430.1
438.6
433.8
464.8
444.1
456.0
16.1
16.4
15.3
6.9
10.2
10.6
7.0
14.9
12.7
4.2
23.3
13.4
12.2
20.6
11.3
17.2
7.2
15.8
11.0
10.8
41.0
33.9
15.1
447.6
427.4
422.5
436.1
438.2
449.2
443.9
435.9
402.7
438.2
481.6
412.4
431.7
441.9
423.9
477.3
421.0
408.0
459.4
399.1
581.7
440.3
477.9
72.3
77.4
84.2
25.9
42.3
46.4
32.4
90.2
77.3
16.8
137.9
79.8
38.4
29.3
52.6
96.8
42.1
58.3
53.6
38.5
210.8
25.7
71.1
1.32267)
0.0614
0.0626
0.0626
0.0630
0.0632
0.0634
0.0635
0.0635
0.0637
0.0637
0.0637
0.0638
0.0640
0.0640
0.0642
0.0642
0.0643
0.0645
0.0645
0.0645
0.0647
0.0647
0.0649
0.0650
0.0664
0.0671
0.0677
2.1
2.1
2.2
2.4
1.0
2.5
1.6
2.9
1.3
1.9
6.0
2.9
2.0
2.9
1.5
3.9
2.2
3.8
1.2
1.9
3.5
1.7
1.3
1.4
1.9
3.1
1.5
0.79
0.70
0.72
0.58
0.37
0.36
0.72
0.83
0.34
0.77
0.77
0.89
0.65
0.52
0.44
0.95
0.93
0.88
0.57
0.70
0.70
0.57
0.43
0.56
0.71
0.80
0.56
384.3
391.3
391.4
394.1
395.2
396.3
396.9
397.0
398.0
398.2
398.3
398.8
400.1
400.1
401.0
401.4
401.9
403.1
403.1
403.2
403.9
404.1
405.3
406.1
414.2
418.9
422.1
7.9
7.8
8.5
9.3
3.9
9.6
6.2
11.1
5.0
7.2
23.2
11.3
7.7
11.1
5.9
15.4
8.6
14.9
4.8
7.5
13.7
6.6
5.1
5.4
7.7
12.5
6.2
386.2
400.7
391.7
391.0
402.3
393.9
400.5
400.4
396.7
395.1
394.2
399.5
403.8
397.0
398.8
403.6
404.1
401.4
405.7
408.1
400.7
403.3
410.1
402.3
414.9
430.1
418.8
8.6
9.7
10.1
13.5
9.3
22.5
7.3
11.5
12.5
7.9
25.6
10.8
10.2
17.9
11.4
13.8
7.9
14.4
7.2
9.2
16.5
9.9
10.1
8.2
9.1
13.4
9.3
397.0
455.2
393.6
372.4
443.2
379.9
420.8
420.2
389.2
376.5
370.2
403.5
425.3
378.5
386.1
416.4
416.9
391.7
420.4
435.5
382.6
399.2
436.9
379.9
418.9
490.4
400.5
36.5
46.4
48.8
76.2
57.9
144.3
34.4
43.0
80.7
34.5
113.4
33.3
51.8
104.7
69.9
29.0
19.0
47.0
39.8
43.4
80.0
54.7
60.3
45.8
41.9
50.3
50.4
0.0542
0.0643
0.0674
0.0683
0.0683
0.0684
0.0686
0.0687
0.0688
0.0689
0.0689
0.0691
0.0693
0.0693
0.0693
0.0694
0.0694
0.0694
0.0698
0.0698
0.0699
0.0700
0.0700
0.0701
0.0704
0.0722
0.0744
2.4
3.0
2.4
1.4
1.2
1.0
1.5
1.1
1.2
1.8
2.2
1.3
1.5
1.1
2.8
0.7
2.2
1.4
1.3
2.0
2.2
1.6
3.8
1.3
3.7
2.0
5.9
0.92
0.55
0.66
0.42
0.36
0.32
0.17
0.36
0.36
0.37
0.50
0.36
0.68
0.12
0.56
0.10
0.46
0.33
0.31
0.56
0.52
0.40
0.25
0.39
0.79
0.40
0.51
340.0
401.8
420.7
425.6
425.7
426.5
427.7
428.2
429.1
429.2
429.7
430.9
431.8
431.8
431.9
432.4
432.6
432.6
435.0
435.0
435.4
435.9
436.4
436.5
438.7
449.4
462.7
8.0
11.6
9.8
5.9
4.8
4.2
6.3
4.7
4.8
7.4
9.1
5.6
6.1
4.8
11.8
2.8
9.3
5.7
5.6
8.3
9.3
6.7
16.2
5.6
15.6
8.8
26.6
349.3
390.3
413.2
433.4
435.7
421.3
429.5
427.1
422.2
439.0
436.6
426.1
426.4
426.5
430.7
431.0
438.2
426.6
431.2
427.0
435.8
429.9
459.7
428.5
433.3
456.1
455.1
7.8
17.7
12.4
12.0
11.3
10.9
30.4
11.1
11.2
17.0
15.7
12.8
7.5
32.1
17.6
22.7
17.4
14.6
14.9
12.2
14.9
13.8
57.7
11.8
16.4
18.8
43.0
411.8
322.9
371.8
474.7
488.9
392.8
439.6
420.8
385.0
490.3
473.3
400.6
397.3
398.0
424.5
423.7
468.0
394.5
410.9
383.5
437.9
398.0
577.5
386.0
404.7
490.1
416.6
23.7
103.7
61.7
68.1
65.8
66.9
190.5
66.2
68.2
97.6
84.7
76.9
35.5
205.5
92.4
143.6
96.1
89.0
90.3
65.1
79.8
81.1
329.9
69.5
63.7
103.5
226.2
imal: 55.58607, 131.34565)
0.0352
1.8
0.0378
0.8
0.0417
3.8
0.0442
1.4
0.0384
1.5
0.94
0.49
0.32
0.85
0.82
223.3
239.1
263.2
278.5
243.0
3.9
1.8
9.9
3.9
3.6
227.1
241.1
300.6
281.2
247.3
3.9
3.3
31.4
4.2
4.0
266.6
260.1
602.3
303.2
288.1
15.3
30.9
248.2
20.5
23.8
imal: 55.60782, 131.35703)
0.0151
0.9
0.0216
6.6
0.0247
3.0
0.0375
2.2
0.0380
1.8
0.0384
1.7
0.0387
0.6
0.0398
1.6
0.0398
4.0
0.0398
1.1
0.0399
2.7
0.0400
1.1
0.0402
5.1
0.0408
2.4
0.10
0.34
0.50
0.85
0.73
0.75
0.34
0.50
0.84
0.22
0.76
0.35
0.40
0.76
96.8
137.7
157.2
237.0
240.7
242.7
244.6
251.5
251.6
251.7
252.1
253.0
254.3
257.5
0.9
9.1
4.7
5.1
4.4
3.9
1.5
3.9
9.9
2.8
6.7
2.6
12.7
6.0
89.6
135.3
164.8
242.7
242.7
245.1
244.6
256.2
256.2
261.1
249.2
255.7
246.7
262.7
8.0
24.4
9.3
5.6
5.4
4.8
4.1
7.1
10.8
11.6
8.0
6.9
28.3
7.2
-100.5
93.2
275.1
297.7
261.9
268.7
244.6
300.2
298.5
346.1
221.6
280.7
175.3
308.9
228.4
431.8
121.0
31.3
39.1
33.1
40.5
62.1
58.1
111.1
54.6
65.3
278.0
46.5
0.0409
0.0409
0.0410
0.0410
0.0410
0.0411
0.0411
0.0411
0.0414
0.0414
0.0414
0.0414
0.0419
0.0420
0.0420
0.0421
0.0423
0.0423
0.0423
0.0425
0.0449
0.0460
0.0465
0.0475
0.0560
0.0571
0.0663
0.0695
0.2601
2.7
1.8
1.9
1.3
1.4
2.5
3.9
1.4
0.5
1.4
0.6
0.8
1.2
6.4
2.6
2.3
1.5
3.9
4.4
1.3
1.2
1.7
2.4
1.3
1.1
5.1
3.7
1.7
5.8
0.96
0.63
0.63
0.46
0.60
0.53
0.82
0.53
0.32
0.27
0.19
0.35
0.47
0.89
0.65
0.22
0.40
0.30
0.46
0.17
0.33
0.42
0.95
0.19
0.34
0.69
0.52
0.30
0.90
258.3
258.6
258.8
259.1
259.1
259.4
259.5
259.7
261.4
261.5
261.6
261.6
264.7
265.0
265.4
265.7
266.8
266.8
266.9
268.6
283.3
289.8
292.9
299.2
351.0
357.8
413.9
433.4
1490.5
6.9
4.5
4.8
3.4
3.4
6.2
9.8
3.6
1.4
3.6
1.5
2.1
3.2
16.7
6.6
6.1
3.9
10.1
11.5
3.5
3.3
4.8
7.0
3.8
3.9
17.9
14.9
7.1
77.2
261.4
255.0
258.6
255.3
257.0
262.0
262.2
262.2
260.1
266.2
264.1
264.9
264.9
268.3
272.7
266.7
276.8
249.6
275.4
267.0
283.6
291.5
305.3
287.8
343.2
345.5
425.5
437.6
1572.9
6.5
6.3
6.9
6.6
5.1
10.7
10.9
6.2
3.8
12.2
7.1
5.4
6.1
17.1
9.4
24.4
9.0
28.7
23.2
19.1
8.8
10.2
6.8
17.0
9.6
21.9
25.0
20.2
51.5
289.6
221.6
256.6
220.3
237.3
285.6
286.6
284.4
248.9
307.5
285.7
294.3
266.6
297.2
335.5
275.2
361.9
90.9
348.8
253.1
285.4
304.7
401.1
196.5
290.7
263.4
489.2
459.8
1685.4
18.1
50.0
53.8
60.0
41.0
90.3
62.5
52.4
36.4
114.3
68.4
49.5
52.6
75.9
67.3
233.2
76.7
294.6
193.7
184.3
76.7
83.6
18.1
154.9
71.1
124.4
136.0
120.7
51.0
56.21356, 131.56098)
0.0086
1.8
0.0223
2.9
0.0313
1.0
0.5
0.0535
0.0545
1.9
0.0589
0.7
0.0626
3.4
0.0640
0.8
0.0655
3.4
0.0662
1.6
0.0673
1.9
0.1036
1.2
0.1207
2.5
0.1309
1.8
0.1328
4.5
0.1425
1.4
0.1470
2.9
0.1471
1.7
0.1590
1.4
0.1483
2.9
0.1698
2.9
0.70
0.85
0.55
0.53
0.88
0.50
0.97
0.83
0.95
0.92
0.91
0.88
0.89
0.90
0.98
0.88
0.83
0.90
0.89
0.89
0.96
55.2
142.4
198.7
335.7
342.0
369.0
391.6
400.0
408.8
412.9
419.8
635.7
734.8
793.1
803.6
858.9
883.9
884.6
950.9
891.5
1010.9
1.0
4.1
2.0
1.7
6.2
2.4
13.1
3.1
13.4
6.5
7.8
7.2
17.1
13.7
33.6
11.3
24.3
13.9
12.6
23.8
27.0
56.9
148.1
346.5
344.5
348.9
376.9
397.3
403.9
413.0
417.0
434.8
637.1
745.0
846.9
842.0
882.2
912.8
914.7
974.5
939.1
1030.3
1.4
4.8
5.5
2.9
6.2
4.1
11.7
3.3
12.1
6.0
7.4
6.3
14.6
11.8
26.0
9.3
21.5
11.3
10.0
19.8
19.4
130.7
240.2
1512.5
404.2
395.2
425.4
430.4
426.6
436.6
439.4
514.7
642.0
775.7
990.7
944.6
940.9
983.4
987.9
1027.8
1052.5
1071.9
42.4
42.7
29.7
18.9
22.0
25.4
18.9
12.4
24.4
15.5
19.0
13.6
26.5
18.6
18.9
15.2
40.9
16.9
14.7
29.9
16.6
0.1665
0.1759
0.1637
0.1455
0.1466
0.1810
0.1790
0.1573
0.1672
0.1656
0.1949
0.1935
0.1641
0.1918
0.1834
0.1795
0.1666
0.1790
0.2090
0.2269
0.2109
0.2110
0.2159
0.1921
0.2206
0.2260
0.2352
0.2155
0.2363
0.2420
0.2371
0.2329
0.2722
0.2868
0.2543
0.2454
0.2300
0.2414
0.2606
0.2575
0.2823
0.2831
0.2628
0.2942
0.3045
0.3048
0.2619
0.2943
0.2902
0.3207
0.3437
0.3569
5.0
1.8
5.3
1.8
3.8
1.9
2.0
2.1
2.2
1.4
1.5
1.5
1.6
0.9
4.6
3.7
3.7
2.5
1.0
2.7
2.5
1.6
1.5
3.4
2.4
1.8
0.7
1.8
1.8
2.5
1.1
2.2
2.1
1.5
1.4
2.5
3.8
0.7
1.2
1.2
2.3
1.5
2.8
1.2
1.9
2.2
3.1
1.1
1.0
4.1
2.9
2.3
0.98
0.95
0.99
0.74
0.95
0.75
0.93
0.95
0.94
0.82
0.79
0.92
0.70
0.87
0.99
0.98
0.94
0.93
0.75
0.96
0.95
0.93
0.81
0.59
0.88
0.91
0.61
0.94
0.91
0.57
0.78
0.93
0.93
0.86
0.90
0.91
0.99
0.50
0.78
0.88
0.75
0.89
0.89
0.91
0.88
0.94
0.98
0.87
0.70
0.98
0.97
0.91
993.0
1044.3
977.2
875.9
881.8
1072.5
1061.4
941.8
996.8
988.1
1148.1
1140.2
979.4
1131.1
1085.6
1064.3
993.6
1061.5
1223.3
1318.4
1233.4
1234.3
1260.0
1132.8
1285.3
1313.4
1361.5
1258.1
1367.3
1397.3
1371.8
1349.4
1551.8
1625.7
1460.9
1414.6
1334.7
1393.8
1492.8
1477.0
1602.9
1606.9
1504.3
1662.4
1713.6
1715.3
1499.7
1662.9
1642.4
1792.9
1904.5
1967.3
46.3
17.6
48.2
14.4
31.5
18.6
19.4
18.1
20.3
13.1
15.5
15.3
14.3
9.4
46.2
36.0
33.8
24.2
11.1
32.8
27.7
17.7
17.1
35.2
28.1
21.8
8.8
20.6
22.4
31.8
13.6
27.3
29.3
21.2
18.6
31.6
46.2
8.2
15.5
15.6
32.7
21.8
38.1
18.1
28.0
33.6
41.3
15.5
15.1
64.6
47.5
38.8
1018.4
1055.5
1009.3
936.7
942.8
1079.7
1073.4
990.3
1033.2
1036.4
1146.2
1146.0
1036.8
1148.4
1118.3
1107.5
1059.4
1128.3
1245.4
1320.3
1274.6
1281.7
1299.2
1223.2
1340.6
1361.2
1398.4
1339.9
1422.1
1458.0
1464.4
1454.4
1583.8
1627.1
1531.2
1504.6
1456.8
1499.9
1561.0
1556.3
1652.6
1659.2
1605.2
1698.3
1731.7
1777.5
1659.5
1763.0
1770.7
1874.9
1962.3
2021.0
32.9
12.6
34.4
14.5
24.7
16.7
14.2
13.7
15.2
11.4
12.8
10.9
14.6
7.1
31.6
25.3
25.6
18.0
9.6
21.1
18.9
12.3
13.5
41.1
20.5
15.1
8.9
14.3
15.2
34.2
10.9
18.6
18.2
13.9
12.5
21.5
30.0
10.2
11.9
10.7
25.0
14.0
25.7
11.1
17.5
20.0
25.7
10.2
12.5
36.1
25.7
22.1
1073.3
1078.9
1079.7
1082.5
1088.2
1094.3
1097.9
1099.2
1111.2
1139.7
1142.8
1156.9
1159.9
1181.3
1182.4
1193.3
1197.8
1259.0
1283.7
1323.5
1344.8
1362.1
1364.6
1386.3
1430.1
1437.1
1455.1
1473.1
1505.1
1547.7
1601.3
1611.2
1626.6
1629.0
1629.9
1633.8
1639.7
1653.2
1654.6
1665.7
1716.3
1726.2
1740.3
1743.0
1753.5
1851.3
1868.1
1883.8
1925.6
1967.0
2023.8
2076.2
19.0
12.1
16.2
32.0
24.4
33.5
16.3
13.5
16.3
20.1
22.8
12.3
31.5
10.0
11.5
15.5
25.4
18.5
17.4
15.0
15.6
12.0
20.7
89.8
25.1
16.3
17.8
12.9
15.4
67.9
16.4
16.0
15.1
16.1
12.8
21.2
11.3
21.0
17.4
11.6
37.2
14.2
26.7
10.0
18.2
15.0
10.7
10.9
19.2
15.9
12.2
18.4
0.4730
0.4060
0.4415
0.4746
0.4276
3.7
3.8
2.1
1.1
1.8
0.97
0.94
0.78
0.62
0.94
2496.5
2196.6
2357.6
2503.6
2294.9
75.9
70.2
42.2
22.7
35.4
2611.1
2471.4
2563.6
2685.8
2595.2
35.3
37.2
25.4
16.5
18.3
2701.2
2705.9
2730.9
2825.9
2838.8
14.0
22.9
27.8
22.4
10.9
0.0088
0.0088
0.0094
0.0095
0.0298
0.0414
0.0425
0.0430
0.0460
0.0539
0.0584
0.0591
0.0628
0.0631
0.0651
0.0665
0.0672
0.0679
0.0681
0.0696
0.0760
0.0875
0.0919
0.1078
0.1502
0.1583
0.1616
0.1603
0.1657
0.1737
0.1801
0.1656
0.1768
0.1781
0.1860
0.1903
0.1854
0.1904
0.1789
0.1881
0.1754
0.1821
0.1921
0.2002
0.1961
1.4
0.9
2.5
3.2
3.2
8.9
3.8
6.0
4.9
1.5
1.9
3.4
6.1
2.1
6.2
1.7
1.0
4.8
3.4
2.7
4.5
6.7
2.0
9.4
2.2
2.8
1.8
3.3
0.9
5.4
3.7
2.8
2.0
4.4
4.9
4.0
3.2
7.2
1.8
1.2
4.9
4.3
6.6
2.2
4.4
0.20
0.68
0.14
0.30
0.89
0.98
0.76
0.73
0.76
0.93
0.99
0.98
0.83
0.67
1.00
0.83
0.91
0.74
0.98
0.71
0.31
0.96
0.96
0.97
0.88
0.82
0.49
0.96
0.79
0.66
0.90
1.00
0.54
0.97
0.94
0.89
0.85
0.79
0.48
0.94
0.98
0.93
0.74
0.99
0.96
56.5
56.7
60.4
61.0
189.0
261.2
268.4
271.6
290.1
338.2
365.7
370.1
392.9
394.7
406.5
415.2
419.1
423.8
424.6
433.8
472.3
540.7
566.6
659.8
902.0
947.5
965.7
958.4
988.6
1032.2
1067.4
987.8
1049.2
1056.7
1099.6
1123.0
1096.5
1123.6
1060.8
1110.9
1041.5
1078.5
1132.6
1176.2
1154.2
0.8
0.5
1.5
1.9
5.9
22.7
9.9
15.9
14.0
4.8
6.7
12.1
23.3
8.2
24.4
6.8
3.9
19.5
14.0
11.4
20.5
34.9
11.1
59.1
18.9
24.3
15.8
29.6
8.5
51.4
36.0
26.1
18.9
43.0
49.7
41.6
32.7
74.5
17.3
12.2
47.5
42.4
68.8
23.8
46.7
57.9
58.0
58.2
65.6
196.4
331.4
272.3
277.7
591.6
349.5
371.4
380.5
396.4
396.8
410.9
420.5
423.0
424.2
426.2
424.9
450.3
658.4
565.1
666.0
908.1
949.3
980.4
980.0
1001.5
1033.1
1070.1
1024.0
1074.5
1082.0
1113.1
1128.9
1113.1
1131.5
1094.8
1130.9
1103.6
1148.0
1191.9
1226.0
1215.2
3.9
0.8
9.8
6.8
6.4
25.6
11.9
19.9
29.2
4.7
6.0
11.0
24.3
10.4
20.9
7.0
3.6
22.2
12.1
13.3
52.1
34.0
9.3
47.4
15.2
20.8
22.4
21.8
7.4
52.9
26.9
18.4
24.2
30.2
35.3
30.9
25.7
62.5
24.9
8.7
33.9
31.5
63.0
15.9
32.5
116.4
114.9
-31.1
235.2
285.6
859.0
306.8
330.2
2023.1
425.7
407.1
444.5
417.3
408.5
436.1
449.7
444.6
426.8
434.8
376.7
339.4
1085.9
558.9
687.3
923.1
953.6
1013.5
1028.8
1029.9
1035.0
1075.5
1102.2
1126.1
1133.4
1139.7
1140.2
1145.5
1146.8
1162.9
1169.7
1228.0
1281.8
1301.1
1314.8
1325.3
161.7
24.2
419.9
235.1
37.3
39.0
73.9
126.8
75.4
12.6
7.0
16.9
92.9
52.6
7.3
25.0
9.5
95.9
14.9
60.9
308.6
39.3
13.0
49.3
24.3
39.5
62.9
20.4
14.5
123.8
35.3
4.3
61.3
21.7
34.5
40.8
39.5
111.6
64.9
8.6
19.0
31.8
117.7
6.9
23.3
0.2232
0.2281
0.0913
0.2191
0.2301
0.2460
0.2334
0.2504
0.0965
0.2383
0.2323
0.2480
0.2403
0.2351
0.2361
0.2579
0.2569
0.2246
0.2854
0.2392
0.2655
0.2397
0.2702
0.2418
0.2851
0.2999
0.2943
0.3134
0.2990
0.2849
0.3917
0.5042
0.4380
0.5468
2.4
2.2
5.7
4.0
3.1
3.7
3.2
1.5
5.8
2.2
1.9
3.2
2.4
4.2
4.8
1.7
4.1
1.5
2.5
7.5
3.8
4.7
4.9
6.0
3.6
2.0
1.9
1.1
2.2
2.0
3.5
3.6
2.6
2.0
0.72
0.93
0.99
0.73
0.99
0.97
0.99
0.97
0.97
0.96
0.91
0.97
1.00
0.93
0.99
1.00
0.98
0.98
0.94
0.98
1.00
0.99
1.00
1.00
0.98
0.92
0.98
0.92
0.99
0.96
0.98
0.98
1.00
0.98
1298.7
1324.7
563.3
1276.9
1334.9
1418.0
1352.2
1440.6
593.7
1377.7
1346.4
1428.0
1388.4
1361.0
1366.6
1479.1
1473.7
1306.0
1618.4
1382.3
1518.1
1385.1
1541.7
1396.3
1617.0
1691.0
1663.2
1757.3
1686.3
1616.0
2130.7
2631.9
2341.9
2812.1
27.7
26.2
30.6
46.4
37.7
46.5
38.5
19.9
32.9
27.5
22.5
41.4
29.5
52.1
59.0
22.7
54.0
17.4
36.4
93.3
51.1
58.6
67.1
75.9
51.8
30.0
27.1
16.7
33.0
28.8
63.1
77.6
50.1
46.3
1311.2
1344.0
759.2
1331.0
1376.7
1431.5
1392.8
1447.3
816.4
1420.2
1403.1
1454.6
1431.9
1415.5
1420.4
1489.2
1532.2
1428.1
1621.3
1490.0
1573.4
1492.6
1597.7
1523.9
1671.1
1715.0
1712.0
1773.3
1740.5
1792.2
2344.8
2652.4
2549.4
2903.1
24.0
17.6
30.7
40.6
23.7
28.8
24.2
12.3
33.5
17.6
15.4
25.7
18.2
34.8
37.0
13.5
33.2
11.5
22.0
59.9
30.3
37.0
39.6
47.9
30.2
18.0
15.6
9.8
18.6
17.6
32.6
34.5
23.9
19.8
1331.7
1374.8
1389.5
1419.0
1442.0
1451.5
1455.4
1457.1
1484.1
1484.3
1490.3
1493.8
1497.1
1498.5
1502.0
1503.4
1613.8
1615.0
1625.1
1646.8
1648.4
1648.9
1672.3
1706.0
1739.6
1744.5
1772.2
1792.1
1806.1
2003.8
2536.7
2668.2
2719.0
2966.9
43.5
16.7
16.6
71.2
6.7
16.3
8.7
7.5
26.9
12.1
15.6
14.8
4.1
31.2
13.3
3.0
16.6
5.7
17.7
28.0
5.1
10.0
7.7
7.9
13.1
15.3
6.9
8.1
4.6
10.0
12.9
12.4
2.7
5.9
0.0106
0.0113
0.0122
0.0128
0.0130
0.0131
0.0131
0.0132
0.0139
0.0140
0.0145
0.0146
0.0149
0.0151
0.0153
0.0160
2.1
1.0
3.2
1.5
1.8
4.2
2.6
2.3
7.5
4.0
1.2
3.6
1.1
1.0
1.9
4.2
0.95
0.73
0.96
0.62
0.90
0.86
0.88
0.78
0.98
0.77
0.82
0.67
0.72
0.39
0.94
0.95
67.7
72.2
78.1
81.7
83.5
83.6
83.9
84.2
88.8
89.8
92.6
93.4
95.4
96.5
97.7
102.1
1.4
0.7
2.5
1.2
1.5
3.5
2.2
1.9
6.6
3.6
1.1
3.4
1.1
0.9
1.9
4.3
68.8
72.2
79.5
83.8
85.5
81.7
87.1
89.4
89.8
93.3
92.7
104.7
96.4
100.4
99.0
101.1
1.5
0.9
2.5
1.9
1.7
3.9
2.5
2.5
6.6
4.7
1.3
5.4
1.4
2.4
1.9
4.3
108.1
73.2
120.8
144.1
141.3
27.0
176.4
228.2
115.8
182.1
95.2
370.2
121.6
194.7
131.1
76.6
15.6
21.8
23.0
43.1
20.2
60.5
33.1
43.2
33.6
77.3
20.0
91.2
25.6
53.0
15.7
32.4
0.0162
0.0171
0.0188
0.0188
0.0252
0.0281
0.0284
0.0300
0.0314
0.0316
0.0319
0.0325
0.0326
0.0332
0.0332
3.3
3.0
6.4
2.0
7.1
6.9
1.0
1.5
1.9
2.4
4.4
3.8
1.2
1.0
2.8
0.98
0.63
0.99
0.95
0.95
1.00
0.88
0.90
0.92
0.97
0.96
0.99
0.89
0.81
0.96
103.7
109.6
119.9
119.9
160.2
178.8
180.7
190.7
199.0
200.4
202.3
206.2
206.7
210.2
210.8
3.4
3.3
7.6
2.4
11.3
12.2
1.9
2.9
3.7
4.8
8.7
7.7
2.5
2.1
5.9
108.4
111.5
123.9
122.8
168.6
190.9
182.3
192.9
200.6
202.4
203.1
207.9
207.6
213.1
207.9
3.4
5.0
7.5
2.4
11.6
12.0
2.0
3.0
3.7
4.6
8.4
7.2
2.6
2.4
5.6
211.9
152.8
201.2
180.0
287.8
343.3
202.7
220.4
218.4
226.0
212.5
227.5
218.3
245.1
174.5
16.3
86.2
16.4
15.9
53.9
14.0
13.2
17.0
18.2
14.4
28.2
13.2
14.7
17.0
18.8
0.0130
0.0135
0.0136
0.0138
0.0139
0.0139
0.0140
0.0142
0.0143
0.0143
0.0147
0.0148
0.0148
0.0149
0.0150
0.0161
0.0173
0.0222
0.0252
0.0254
0.0272
0.0277
0.0277
0.0281
0.0287
0.0310
0.0546
3.5
0.9
3.0
2.6
2.2
1.0
2.3
2.6
1.2
1.9
1.0
2.9
2.6
0.5
3.8
3.2
5.0
2.3
4.7
1.6
1.0
1.8
1.4
1.1
2.8
5.6
1.7
0.89
0.74
0.98
0.75
0.96
0.25
0.90
0.90
0.69
0.66
0.88
0.99
0.97
0.28
0.36
0.96
0.96
0.97
0.99
0.93
0.75
0.89
0.79
0.74
0.95
0.99
0.88
83.3
86.2
87.0
88.5
88.9
89.2
89.7
90.8
91.2
91.4
94.1
94.5
94.9
95.3
95.9
102.7
110.6
141.3
160.7
161.6
172.9
176.2
176.2
178.6
182.2
196.5
342.6
2.9
0.8
2.6
2.3
1.9
0.9
2.0
2.4
1.1
1.7
0.9
2.8
2.4
0.5
3.6
3.2
5.5
3.2
7.5
2.5
1.7
3.2
2.5
2.0
5.0
10.9
5.8
87.8
87.2
87.7
89.9
87.8
88.0
90.3
90.3
91.0
93.8
90.8
94.5
95.8
89.8
108.2
100.4
105.3
140.9
172.2
163.7
173.7
177.2
177.2
180.5
182.0
199.1
334.2
3.3
1.0
2.6
2.9
1.9
3.3
2.2
2.5
1.6
2.6
1.0
2.7
2.4
1.6
10.9
3.2
5.2
3.1
7.6
2.6
2.1
3.3
3.0
2.6
4.9
10.3
5.6
210.3
115.6
108.7
126.4
57.7
56.6
106.5
78.1
85.0
157.4
5.8
93.1
119.7
-54.6
388.3
46.7
-11.2
135.0
334.1
194.3
185.2
191.4
191.1
205.8
179.5
229.4
276.3
42.0
19.6
14.5
53.1
15.9
89.9
25.5
29.4
31.2
51.0
12.9
12.0
14.6
42.2
221.9
22.3
36.6
13.6
15.7
14.9
19.9
21.3
26.4
24.2
21.5
22.1
21.4
1.1
5.8
3.5
7.0
1.3
1.8
0.24
0.13
0.10
0.18
0.22
0.42
69.0
83.6
83.6
84.1
84.8
84.9
0.8
4.8
2.9
5.9
1.1
1.5
66.5
82.1
88.9
74.8
79.8
76.6
3.0
36.4
28.6
28.4
4.4
3.2
-21.5
38.9
234.1
-211.6
-64.8
-173.8
110.2
1149.1
791.9
1006.0
135.7
97.8
651, 131.80678)
0.0108
0.0131
0.0131
0.0131
0.0132
0.0133
0.0133
0.0133
0.0133
0.0133
0.0133
0.0134
0.0134
0.0134
0.0135
0.0135
0.0135
0.0135
0.0135
0.0135
0.0135
0.0135
0.0135
0.0135
0.0136
0.0136
0.0136
0.0136
0.0137
0.0137
0.0137
0.0137
0.0137
0.0137
0.0138
0.0138
0.0138
0.0139
0.0139
0.0139
0.0139
0.0139
0.0140
0.0140
0.0140
0.0140
0.0140
0.0141
0.0141
0.0141
0.0142
0.0142
0.0142
0.0151
0.0152
1.5
2.4
1.3
1.6
1.1
3.1
2.7
1.6
0.7
1.8
1.9
1.1
1.3
1.6
2.7
1.1
1.8
5.8
1.3
0.5
1.3
1.0
1.9
1.3
0.6
4.8
6.2
1.6
1.2
1.7
0.9
8.0
0.9
2.3
2.5
0.9
1.6
0.6
4.9
5.1
1.6
5.4
2.0
0.8
4.5
5.8
0.9
3.9
1.8
0.57
0.45
0.24
0.16
0.36
0.19
0.28
0.11
0.15
0.31
0.24
0.19
0.39
0.12
0.22
0.40
0.16
0.20
0.41
0.28
0.38
0.69
0.42
0.29
0.20
0.18
0.14
0.30
0.34
0.14
0.57
0.37
0.33
0.43
0.46
0.47
0.26
0.31
0.01
0.20
0.24
0.16
0.36
0.14
0.16
0.32
0.73
0.24
0.69
84.9
85.4
85.4
85.4
85.5
85.7
85.9
85.9
86.2
86.2
86.2
86.3
86.3
86.4
86.6
86.6
86.7
86.7
87.2
87.2
87.2
87.2
87.4
87.5
87.5
87.8
87.8
87.9
88.1
88.2
88.5
88.7
88.8
89.0
89.2
89.2
89.4
89.5
89.6
89.6
89.6
90.0
90.2
90.3
90.6
91.0
91.2
96.3
97.0
1.3
2.1
1.1
1.4
0.9
2.6
2.3
1.4
0.6
1.6
1.6
1.0
1.1
1.4
2.3
0.9
1.5
5.0
1.1
0.4
1.1
0.8
1.6
1.1
0.5
4.2
5.4
1.4
1.0
1.5
0.8
7.1
0.8
2.1
2.2
0.8
1.4
0.5
4.3
4.5
1.4
4.9
1.8
0.7
4.1
5.2
0.8
3.8
1.7
84.2
86.0
79.4
79.6
85.6
88.3
82.6
87.6
85.5
85.9
87.5
88.8
89.1
76.8
93.1
86.9
90.8
70.0
87.7
87.6
88.0
87.9
89.2
89.1
86.6
85.8
78.4
85.9
88.6
83.8
89.8
84.0
89.2
87.7
88.3
90.5
93.2
89.7
297.6
96.0
91.4
64.0
91.0
91.4
86.1
103.4
91.6
92.2
98.6
2.1
4.5
4.3
7.9
2.5
14.0
7.7
12.1
4.0
4.9
6.6
5.0
2.8
10.0
10.7
2.3
9.4
19.1
2.5
1.5
2.8
1.2
3.8
3.9
2.5
22.2
34.8
4.5
3.0
9.6
1.4
17.4
2.4
4.6
4.6
1.6
5.3
1.5
#NUM!
23.2
5.9
21.2
5.0
4.8
23.6
17.7
1.1
14.3
2.4
63.0
103.7
-97.9
-92.5
88.4
158.6
-9.9
133.1
64.9
78.8
123.5
156.5
163.2
-212.6
264.5
94.8
199.3
-469.1
102.2
99.1
108.5
106.5
136.8
131.4
61.3
31.6
-201.2
33.1
103.2
-40.3
124.8
-48.7
101.1
51.3
63.6
125.1
192.2
93.6
2620.3
258.2
138.4
-826.8
112.2
120.2
-39.1
401.4
102.0
-12.5
139.1
51.2
114.7
135.4
251.8
67.9
383.0
225.1
337.8
116.0
134.0
180.5
134.1
69.5
337.0
271.0
59.9
247.7
740.8
65.2
41.6
73.0
23.8
94.6
102.3
69.2
645.0
1202.4
125.7
77.9
289.0
30.4
490.6
62.6
118.0
114.9
38.9
134.7
40.0
460.1
578.7
153.1
986.0
126.2
127.7
698.2
384.0
20.9
383.3
44.3
ecimal: 56.23231, 131.93211; )
0.0951
3.7
0.35
585.6
20.6
614.1
48.8
720.3
211.1
0.2185
0.2730
1.8
5.1
0.68
0.96
1274.0
1556.0
20.7
70.2
1263.6
1601.1
19.1
42.5
1246.1
1661.0
37.9
25.9
279, 132.03072)
0.0117
0.0573
0.0544
1.3
1.5
1.9
0.50
0.76
0.92
75.3
359.3
341.7
1.0
5.3
6.3
77.4
362.2
343.8
2.0
6.1
6.0
142.9
380.9
357.5
53.5
28.9
18.1
2.05331)
0.0412
0.0520
0.0579
0.0594
0.0598
0.0599
0.0600
0.0607
0.0613
0.0613
0.0614
0.0619
0.0626
0.0633
4.1
3.9
1.9
1.8
3.2
1.2
1.2
1.2
2.0
2.3
3.1
1.9
4.3
4.2
0.77
0.37
0.28
0.29
0.38
0.27
0.15
0.19
0.38
0.57
0.57
0.29
0.48
0.23
260.1
326.9
362.6
371.9
374.6
375.0
375.8
379.6
383.4
383.5
383.9
387.3
391.4
395.8
10.4
12.3
6.7
6.6
11.5
4.6
4.2
4.6
7.5
8.7
11.4
7.0
16.4
16.0
266.6
345.9
352.6
375.0
400.9
386.1
395.7
377.8
390.2
384.2
387.9
397.6
379.4
438.5
12.5
30.3
20.2
19.6
27.7
14.7
25.9
20.6
17.5
13.1
17.2
21.0
28.6
64.8
324.9
475.5
287.3
393.8
555.6
453.1
514.0
367.1
431.0
388.7
411.4
458.2
307.3
669.4
77.5
212.5
149.0
134.4
169.2
97.8
172.1
144.8
111.4
75.7
98.0
135.3
180.9
381.4
2.88538)
0.0089
0.0094
0.0123
0.0125
0.0127
0.0128
0.0129
0.0131
0.0133
0.0137
0.0141
0.0145
0.0159
0.0163
0.0180
0.0370
0.0395
0.0418
0.0445
0.0475
0.0492
0.0528
0.0553
0.0565
0.0569
0.0570
0.0570
3.4
2.1
0.8
3.2
2.5
1.8
1.5
9.1
3.9
1.1
0.7
2.4
9.7
2.9
2.2
2.3
6.1
4.6
5.7
1.4
2.3
1.3
1.5
0.8
0.6
2.0
3.1
0.79
0.46
0.79
0.97
0.90
0.88
0.91
0.99
0.77
0.71
0.28
0.96
0.91
0.96
0.92
0.94
0.99
0.97
0.99
0.87
0.94
0.84
0.94
0.67
0.61
0.94
0.93
57.2
60.1
78.8
79.9
81.4
82.1
82.5
83.7
85.0
87.8
90.4
92.6
101.7
104.3
115.0
234.4
249.5
264.2
280.7
299.1
309.5
331.7
347.3
354.3
356.9
357.3
357.3
1.9
1.3
0.6
2.6
2.0
1.4
1.2
7.5
3.3
0.9
0.6
2.2
9.8
3.0
2.6
5.4
15.0
11.9
15.7
4.2
6.9
4.2
5.2
2.6
2.1
7.0
10.9
139.2
149.0
79.9
81.2
82.1
83.8
83.9
87.4
91.4
89.9
92.1
95.8
121.6
108.5
122.1
246.3
261.5
274.0
288.6
309.5
320.4
335.1
354.1
358.6
362.6
365.1
357.7
5.6
6.5
0.8
2.6
2.1
1.6
1.3
7.6
4.4
1.3
2.2
2.3
12.2
3.1
2.8
5.4
14.3
11.3
14.5
4.4
6.6
4.4
4.8
3.4
3.0
6.6
10.2
1951.2
1991.3
112.7
118.3
100.9
130.8
124.5
188.7
261.5
143.9
138.5
175.5
531.5
202.3
262.0
361.1
370.6
358.1
352.6
388.5
400.6
358.9
399.1
386.2
399.2
415.1
360.1
46.8
74.1
14.7
17.4
27.6
21.9
16.5
25.7
74.6
25.3
55.2
16.5
94.9
19.6
22.0
19.5
24.1
23.9
18.6
18.1
18.5
19.1
12.1
19.0
17.5
16.5
27.2
0.0576
0.0577
0.0577
0.0579
0.0583
0.0584
0.0585
0.0587
0.0588
0.0590
0.0592
0.0592
0.0595
0.0596
0.0602
0.0604
0.0604
0.0607
0.0635
0.4
1.9
1.6
2.5
1.0
1.3
1.3
1.1
1.8
1.4
1.4
2.0
0.8
1.4
1.7
2.4
3.0
0.6
0.6
0.29
0.89
0.85
0.84
0.47
0.92
0.88
0.77
0.89
0.77
0.92
0.91
0.69
0.85
0.89
0.94
0.96
0.57
0.71
360.8
361.7
361.9
362.8
365.1
366.0
366.7
368.0
368.5
369.5
370.7
371.1
372.4
373.1
376.9
378.0
378.2
380.1
396.8
1.5
6.5
5.7
9.0
3.5
4.7
4.7
4.1
6.4
4.9
5.1
7.3
3.1
5.1
6.2
9.0
10.9
2.2
2.5
368.3
363.5
368.0
362.2
371.8
369.0
368.2
371.3
369.3
371.8
371.9
374.6
372.6
371.8
378.4
379.0
384.2
380.3
402.8
4.5
6.4
5.9
9.2
6.6
4.4
4.6
4.6
6.2
5.5
4.7
6.9
3.8
5.2
5.9
8.2
9.8
3.4
3.0
415.8
375.5
406.8
358.4
413.7
388.1
378.1
391.9
373.9
385.9
379.2
396.9
373.8
364.0
387.8
385.0
420.3
381.8
437.8
31.4
21.7
22.1
36.7
41.7
12.4
15.8
21.0
20.4
25.6
13.1
20.2
20.0
20.0
18.9
19.7
18.2
19.6
14.0
0.0624
0.0632
0.0638
0.0642
0.0654
0.0654
0.0656
0.0661
0.0664
0.0664
0.0666
0.0668
0.0668
0.0668
0.0670
0.0671
0.0672
0.0673
0.0674
0.0675
0.0675
0.0676
0.0678
0.0678
0.0679
0.0681
0.0682
0.0683
0.0685
0.0687
0.0688
3.4
1.0
1.6
1.6
1.0
1.4
2.3
1.5
2.8
3.6
5.6
1.4
1.3
1.1
1.9
2.0
0.9
2.3
4.5
1.1
2.0
1.6
0.6
3.9
1.9
1.3
1.6
1.3
1.1
3.5
1.2
0.27
0.59
0.58
0.66
0.37
0.21
0.88
0.91
0.57
0.52
0.24
0.26
0.69
0.72
0.26
0.67
0.22
0.50
0.47
0.63
0.29
0.56
0.67
0.67
0.92
0.31
0.34
0.68
0.49
0.75
0.24
390.2
394.9
398.5
401.4
408.2
408.3
409.3
412.7
414.2
414.6
415.6
416.7
416.8
416.9
418.4
418.9
419.5
420.0
420.7
420.8
420.9
421.7
422.8
422.9
423.7
424.4
425.0
425.9
427.2
428.1
429.0
12.7
3.8
6.1
6.2
4.0
5.4
9.1
6.2
11.1
14.6
22.6
5.8
5.2
4.6
7.7
8.1
3.7
9.2
18.4
4.5
8.3
6.4
2.3
16.1
7.7
5.3
6.8
5.2
4.5
14.7
5.1
395.4
393.0
400.2
412.0
420.2
410.6
410.3
413.9
413.1
411.0
407.4
413.8
415.7
416.2
405.2
419.0
427.8
409.5
413.3
419.9
421.2
423.9
424.0
412.2
426.8
430.1
419.9
425.3
424.7
421.2
411.2
40.3
5.4
9.1
8.2
9.4
21.7
8.9
5.7
16.5
23.8
80.0
19.2
6.5
5.4
24.1
10.3
14.5
15.3
32.6
6.0
24.5
9.7
2.9
20.0
7.1
14.6
16.6
6.5
7.8
16.2
17.5
426.0
381.3
410.0
471.5
486.8
423.6
415.9
420.2
407.1
390.9
361.6
397.4
409.7
412.1
331.0
419.9
472.4
351.0
372.5
414.6
422.7
435.8
430.6
352.9
443.4
460.8
392.0
421.8
410.8
383.9
313.0
264.6
30.1
50.0
40.1
56.3
139.9
28.3
15.4
89.4
135.6
527.9
122.8
30.8
24.2
158.0
50.0
89.5
89.2
191.0
30.4
151.8
52.0
14.1
99.5
18.4
87.9
101.7
30.7
43.7
69.7
114.6
412)
0.0689
0.0689
0.0689
0.0689
0.0694
0.0694
0.0695
0.0697
0.0697
0.0697
0.0700
0.0700
0.0701
0.0702
0.0704
0.0704
0.0705
0.0705
0.0708
0.0709
0.0714
0.0715
0.0716
0.0718
0.0720
0.0720
0.0723
0.0723
0.0727
0.0737
0.0749
0.0753
0.0754
0.0756
0.0759
0.0792
0.0799
0.0802
0.0814
0.0820
0.0821
0.0825
0.0832
0.0859
0.0895
0.0994
0.1061
0.1562
0.1628
0.1754
0.1678
0.1711
2.1
1.2
2.2
0.8
2.4
2.1
2.2
1.8
1.9
1.4
1.0
1.8
1.5
2.3
1.4
3.8
1.4
2.4
2.7
2.1
0.7
2.7
2.4
1.8
1.5
1.6
1.1
2.4
0.6
1.2
3.9
3.7
2.4
1.0
1.1
6.3
2.4
1.8
1.3
2.6
1.5
1.2
4.4
1.6
3.0
1.0
1.4
3.0
1.3
0.9
4.3
2.0
0.25
0.10
0.34
0.19
0.54
0.22
0.18
0.33
0.65
0.65
0.20
0.26
0.31
0.61
0.38
0.89
0.34
0.46
0.41
0.93
0.57
0.37
0.56
0.46
0.64
0.44
0.48
0.47
0.34
0.21
0.25
0.51
0.84
0.87
0.78
0.60
0.21
0.24
0.19
0.17
0.39
0.84
0.90
0.28
0.55
0.17
0.53
0.71
0.90
0.94
0.91
0.26
429.3
429.5
429.6
429.7
432.6
432.8
433.1
434.1
434.2
434.4
436.0
436.3
437.0
437.1
438.6
438.7
438.9
439.3
440.8
441.8
444.3
445.1
445.9
447.0
448.0
448.3
449.8
449.8
452.7
458.6
465.5
468.1
468.9
469.9
471.5
491.6
495.6
497.2
504.2
508.3
508.4
511.1
515.2
531.3
552.5
611.1
650.0
935.9
972.2
1041.9
1000.1
1018.0
8.8
4.8
9.0
3.4
9.9
8.9
9.4
7.7
7.9
5.9
4.1
7.6
6.4
9.9
6.0
16.2
5.9
10.2
11.7
9.0
3.1
11.7
10.3
7.7
6.3
6.8
4.8
10.6
2.8
5.1
17.4
16.8
10.7
4.6
4.8
29.9
11.4
8.4
6.4
12.7
7.2
6.0
21.6
8.4
15.7
6.0
8.7
26.1
11.7
8.4
39.6
18.7
414.0
402.8
412.1
430.8
421.0
411.3
414.2
427.9
433.7
435.3
448.4
418.0
447.2
436.9
436.4
547.0
432.4
437.6
436.7
437.4
445.7
438.1
443.3
448.8
449.4
453.0
442.7
445.6
453.3
457.2
478.5
469.7
466.3
470.9
471.2
496.0
481.6
494.4
482.7
486.5
500.2
509.6
521.4
535.9
554.9
619.7
659.4
927.7
969.4
1038.9
1014.4
1027.9
28.9
39.6
21.8
14.8
15.1
32.2
43.3
19.2
10.3
7.6
17.3
23.6
17.5
13.6
13.4
18.2
14.3
18.6
23.5
8.1
4.6
26.1
15.5
14.1
8.3
12.9
8.1
18.8
6.8
19.7
58.4
27.6
10.5
4.4
5.1
41.5
43.5
28.7
27.4
57.7
14.9
5.9
19.8
24.2
22.8
27.8
12.9
25.6
9.0
6.1
30.1
49.7
329.6
252.3
315.0
436.9
357.8
292.1
309.9
394.9
430.7
439.7
512.7
318.4
500.2
436.1
424.7
1028.2
398.1
428.5
415.6
414.3
453.1
401.2
429.7
457.8
456.5
476.9
405.9
423.7
456.5
450.0
540.9
477.4
453.6
475.9
469.7
516.4
415.7
481.7
381.9
384.8
463.3
502.7
548.7
555.9
564.6
651.1
691.7
908.2
963.0
1032.6
1045.3
1049.0
186.9
273.1
138.1
92.2
83.1
212.5
286.2
116.4
49.7
36.2
102.9
151.4
101.2
67.7
77.9
40.1
85.7
103.6
134.8
19.1
23.3
152.5
79.8
76.5
38.8
70.2
44.4
103.0
38.5
116.4
324.9
140.3
33.5
12.6
18.5
186.5
248.0
157.2
157.5
331.4
76.9
17.6
46.4
121.7
96.7
126.9
48.3
60.6
12.6
6.5
39.1
149.8
0.1801
0.1647
0.1803
0.2004
0.2026
0.2109
0.2595
0.2239
0.2911
0.2850
0.2813
0.2894
0.2944
0.2860
0.3094
0.3201
0.3234
0.3384
0.3854
0.4557
0.4874
0.5099
1.5
1.2
1.1
3.2
2.2
28.1
1.5
2.0
0.8
1.0
1.8
1.8
1.2
3.9
12.9
1.4
1.4
1.2
2.2
2.5
1.8
1.5
0.82
0.93
0.94
0.55
0.65
1.00
0.75
0.93
0.63
0.52
0.96
0.84
0.98
0.99
1.00
0.93
0.54
0.80
0.83
0.70
0.99
0.96
1067.8
982.6
1068.7
1177.3
1189.0
1233.5
1487.1
1302.3
1647.1
1616.5
1598.0
1638.7
1663.3
1621.4
1737.6
1790.2
1806.4
1878.8
2101.6
2420.6
2559.5
2656.0
15.1
10.9
11.0
34.0
23.7
315.9
19.9
24.0
12.3
13.7
25.6
26.6
17.0
55.3
197.0
21.7
21.9
20.1
39.7
51.0
37.2
32.9
1068.5
1013.7
1073.6
1172.9
1195.7
1251.1
1490.3
1421.1
1630.3
1620.5
1615.1
1638.5
1664.2
1681.0
1773.4
1805.9
1817.5
1880.3
2149.9
2423.0
2624.8
2686.9
12.4
8.2
7.9
39.9
23.4
205.2
15.7
16.8
10.9
14.9
15.2
17.8
9.7
32.0
109.0
12.6
21.8
13.2
23.9
33.4
16.7
14.9
1069.9
1081.5
1083.7
1164.9
1207.7
1281.5
1494.9
1604.0
1608.8
1625.6
1637.3
1638.2
1665.4
1756.1
1815.8
1824.0
1830.3
1882.0
2196.3
2425.0
2675.6
2710.2
21.5
9.1
8.4
94.9
49.6
26.5
25.2
15.4
19.5
29.3
9.9
22.0
4.6
10.1
14.7
9.7
39.4
16.6
26.2
44.0
4.9
7.6
9997)
0.0593
0.0609
0.0616
0.0625
0.0642
0.0644
0.0645
0.0648
0.0652
0.0653
0.0654
0.0655
0.0655
0.0655
0.0656
0.0658
0.0658
0.0659
0.0659
0.0661
0.0662
0.0664
0.0668
0.0669
0.0670
0.0671
0.0671
0.0675
8.9
6.6
1.9
2.5
3.3
2.5
2.3
0.8
2.4
2.3
1.9
4.0
0.8
1.0
1.0
1.8
2.3
1.0
3.6
3.3
1.3
5.6
2.7
1.1
0.7
0.9
2.9
2.4
0.98
0.93
0.54
0.97
0.92
0.61
0.90
0.71
0.83
0.60
0.79
0.82
0.45
0.30
0.87
0.50
0.78
0.30
0.99
0.71
0.64
0.94
0.72
0.57
0.50
0.70
0.85
0.63
371.5
380.8
385.2
390.5
401.2
402.4
402.7
404.8
407.0
407.7
408.1
408.7
408.8
409.2
409.3
410.8
410.8
411.1
411.6
412.9
413.5
414.1
416.8
417.4
418.2
418.5
418.6
421.1
32.1
24.5
6.9
9.3
12.8
9.8
8.9
3.2
9.6
9.0
7.4
16.0
3.1
3.9
3.9
7.3
9.0
4.0
14.3
13.3
5.2
22.6
10.9
4.4
2.9
3.8
11.7
9.9
374.1
386.0
390.3
396.4
407.0
416.8
405.5
408.4
409.2
413.9
408.9
419.3
410.8
411.0
411.1
411.8
411.9
413.2
413.6
418.0
414.1
413.8
418.5
417.5
419.0
417.0
420.4
422.5
28.4
22.8
11.1
8.3
12.0
14.2
8.5
3.9
10.0
13.0
7.9
16.9
5.9
11.0
3.8
12.5
9.8
11.2
12.3
16.2
6.8
20.4
12.9
6.5
4.9
4.6
11.6
13.2
390.1
417.0
420.4
430.7
440.4
497.2
421.6
428.9
421.3
448.9
413.5
478.0
421.8
421.3
420.9
417.4
417.9
425.1
424.5
446.4
417.4
411.9
427.5
417.9
423.3
408.9
430.3
430.2
38.1
56.6
64.3
13.8
31.7
72.5
24.2
18.3
37.3
68.4
32.0
62.2
35.2
69.4
12.2
71.6
40.5
69.8
11.9
74.3
34.2
45.5
58.2
34.7
27.4
21.7
39.6
66.1
0.0677
0.0678
0.0678
0.0680
0.0681
0.0681
0.0685
0.0686
0.0686
0.0687
0.0687
0.0688
0.0688
0.0690
0.0693
0.0694
0.0694
0.0695
0.0695
0.0695
0.0697
0.0699
0.0699
0.0703
0.0708
0.0709
0.0711
0.0718
0.0722
0.0725
0.0727
0.0728
0.0733
0.0733
0.0734
0.0734
0.0734
0.0737
0.0739
0.0742
0.0748
0.0754
0.0755
0.0758
0.0761
0.0762
0.0785
0.0792
0.0795
0.0816
0.0892
0.0901
3.5
1.7
5.2
1.6
1.0
2.7
1.6
1.7
0.6
1.3
0.7
2.3
2.2
3.5
1.7
0.8
0.7
1.3
1.4
1.1
1.0
2.0
0.7
1.3
1.9
0.9
1.3
2.2
1.5
1.4
0.7
1.4
1.9
1.4
1.2
1.7
1.8
1.8
1.6
2.4
2.8
1.3
1.9
1.7
1.3
1.4
1.0
0.7
1.8
1.6
1.9
3.0
0.89
0.19
0.97
0.94
0.80
0.13
0.64
0.40
0.24
0.63
0.50
0.42
0.47
0.22
0.96
0.26
0.38
0.36
0.39
0.22
0.82
0.49
0.28
0.73
0.54
0.41
0.56
0.64
0.36
0.80
0.10
0.80
0.86
0.25
0.57
0.72
0.23
0.65
0.37
0.40
0.36
0.68
0.76
0.61
0.84
0.77
0.80
0.78
0.61
0.37
0.47
0.76
422.3
422.7
423.0
424.0
424.5
424.6
427.4
427.8
427.8
428.3
428.5
428.7
428.9
430.3
432.1
432.5
432.6
433.0
433.1
433.4
434.2
435.3
435.5
438.2
440.9
441.8
442.9
447.3
449.7
451.2
452.5
452.7
455.8
455.9
456.7
456.7
456.8
458.5
459.6
461.6
464.8
468.3
469.0
470.7
472.6
473.4
487.3
491.2
493.2
505.8
550.6
555.9
14.3
7.0
21.2
6.8
3.9
11.0
6.5
6.9
2.7
5.3
3.0
9.6
9.1
14.4
7.2
3.3
2.8
5.4
5.7
4.7
4.2
8.3
3.0
5.6
8.0
3.9
5.5
9.4
6.5
6.0
3.1
6.3
8.2
6.0
5.1
7.7
8.1
7.8
7.2
10.7
12.6
6.0
8.7
7.6
5.8
6.5
4.8
3.3
8.6
7.9
9.9
16.0
421.1
440.9
421.3
426.2
424.8
405.7
431.3
432.1
426.8
430.5
428.6
418.3
434.4
451.7
431.3
437.4
426.4
426.8
432.7
438.3
435.6
439.0
438.9
435.0
443.5
443.4
442.1
450.2
461.6
454.8
454.3
453.5
452.7
463.0
461.5
456.0
449.3
456.0
457.5
447.4
454.0
465.6
467.6
471.1
470.8
474.7
486.0
491.1
505.0
514.0
555.0
555.0
13.5
33.1
18.4
6.1
4.2
69.9
8.7
14.8
9.5
7.0
5.1
18.7
16.4
56.8
6.3
10.6
6.0
12.5
12.3
18.1
4.3
14.2
8.9
6.5
12.6
8.0
8.3
12.4
15.5
6.3
26.1
6.6
7.9
20.8
7.6
8.9
28.5
10.0
16.4
21.8
28.8
7.4
9.6
10.3
5.7
7.0
4.9
3.5
11.7
17.7
17.2
16.9
414.5
536.8
412.0
438.2
426.5
299.9
452.4
455.4
421.3
442.3
428.9
361.1
463.9
562.1
427.2
463.1
393.1
393.8
430.4
464.3
443.1
458.2
456.6
418.3
456.9
452.0
438.0
465.2
521.5
473.0
463.8
457.7
437.2
498.2
485.6
452.1
411.2
443.4
447.3
375.0
399.4
452.3
460.6
472.8
461.5
481.1
480.0
490.6
559.2
551.0
572.9
551.0
39.5
199.6
26.5
12.8
16.3
476.2
42.5
85.8
59.4
34.5
28.3
111.6
90.6
332.5
11.0
63.7
36.0
75.2
71.7
109.9
15.5
77.1
53.1
28.1
65.5
45.2
42.8
58.4
85.8
23.1
157.0
23.8
24.4
119.4
37.5
37.6
171.0
45.8
92.1
124.3
165.0
32.3
37.1
47.9
17.8
26.3
16.9
12.4
50.7
88.8
77.1
56.2
0.0909
0.0916
0.0917
0.0918
0.0918
0.0922
0.0923
0.0952
0.0974
0.0989
0.1057
0.1082
0.1083
0.1125
0.1506
0.1600
0.1595
0.1751
0.1807
0.1723
0.2130
0.1986
0.1874
0.1965
0.2313
0.2301
0.2505
0.2494
0.2741
0.2969
0.2150
0.3359
0.3625
0.3729
0.4834
0.4945
0.4556
0.4684
0.5194
0.5459
1.1
0.7
1.3
1.3
0.9
1.0
0.8
4.3
2.0
1.0
2.6
2.3
4.3
6.5
1.1
1.7
1.5
0.8
3.7
1.7
11.8
1.8
1.9
3.4
1.7
0.6
1.1
1.2
2.2
1.4
3.4
1.8
1.8
1.4
0.7
1.3
1.2
2.8
2.8
1.4
0.36
0.58
0.46
0.71
0.23
0.51
0.42
0.28
0.26
0.30
0.92
0.51
0.98
0.93
0.33
0.81
0.41
0.86
0.90
0.94
0.99
0.38
0.86
0.82
0.94
0.39
0.83
0.68
0.92
0.98
0.95
0.92
0.88
0.86
0.90
0.94
0.88
1.00
0.99
0.98
560.8
564.9
565.8
565.9
566.1
568.2
568.9
586.3
599.0
607.9
647.6
662.3
663.1
687.0
904.3
956.7
953.9
1040.0
1070.8
1024.7
1244.8
1167.9
1107.2
1156.3
1341.2
1335.3
1441.1
1435.4
1561.8
1676.1
1255.5
1866.9
1993.9
2043.2
2542.1
2590.1
2420.1
2476.7
2696.8
2808.1
5.7
3.6
7.0
6.9
4.7
5.5
4.3
23.9
11.2
5.5
15.8
14.5
26.9
42.3
9.4
15.3
13.0
8.1
36.5
16.6
133.6
19.3
19.4
36.0
21.0
7.1
14.0
15.3
30.4
21.3
38.6
29.5
31.4
24.9
15.3
28.7
23.8
57.0
61.1
32.7
561.4
567.6
558.0
564.4
563.3
572.4
566.5
605.2
596.6
614.5
647.6
678.2
659.6
694.3
913.6
956.3
962.3
1042.2
1072.4
1042.8
1200.6
1162.6
1124.9
1167.9
1351.7
1352.6
1446.0
1444.1
1586.1
1684.3
1455.6
1884.2
1996.1
2061.9
2551.4
2591.0
2516.8
2545.9
2795.3
2907.2
12.5
5.0
12.2
7.8
16.2
8.7
8.1
69.1
34.1
14.4
13.4
22.2
21.1
35.2
20.6
13.2
22.6
6.4
27.1
12.1
83.8
33.3
15.1
28.6
13.8
11.1
10.1
13.4
19.1
12.1
27.5
17.0
18.1
14.5
7.5
13.3
12.5
26.0
26.5
14.0
563.9
578.4
526.3
558.1
552.0
589.1
556.9
676.5
587.5
638.7
647.4
731.2
647.8
717.8
936.1
955.4
981.6
1046.9
1075.6
1081.0
1121.9
1152.7
1159.2
1189.5
1368.3
1380.2
1453.1
1456.9
1618.7
1694.6
1761.2
1903.3
1998.3
2080.6
2558.7
2591.6
2595.7
2601.6
2867.1
2976.6
59.0
20.4
55.3
27.9
79.5
37.1
36.9
312.2
158.6
63.9
24.2
81.5
18.9
55.0
66.1
25.7
67.6
10.2
35.3
12.5
24.8
88.4
22.4
46.0
12.4
26.3
14.1
24.2
17.1
5.0
20.3
14.1
17.3
14.6
5.9
7.8
10.8
3.7
4.7
4.1
3691)
0.0488
0.0507
0.0609
0.0628
0.0634
0.0645
0.0651
0.0651
0.0652
0.0653
6.4
3.0
5.9
1.4
1.4
5.5
2.9
2.6
1.2
1.9
0.99
0.49
0.87
0.95
0.36
0.78
0.93
0.27
0.93
0.98
307.3
319.1
380.8
392.8
396.3
402.8
406.6
406.7
407.2
407.8
19.2
9.3
21.8
5.5
5.5
21.5
11.5
10.4
4.7
7.7
319.9
330.1
393.5
396.7
381.9
411.9
411.5
427.7
410.0
410.5
17.8
17.2
22.1
5.0
12.4
23.9
10.7
34.3
4.4
6.7
413.0
408.9
468.5
419.7
295.5
463.2
439.1
542.2
425.8
425.3
23.5
119.5
73.5
10.3
83.0
97.3
26.3
207.4
10.6
9.6
0.0654
0.0656
0.0656
0.0656
0.0666
0.0668
0.0670
0.0672
0.0675
0.0677
0.0677
0.0678
0.0678
0.0678
0.0679
0.0679
0.0679
0.0680
0.0681
0.0684
0.0684
0.0684
0.0685
0.0686
0.0686
0.0688
0.0688
0.0690
0.0693
0.0693
0.0696
0.0698
0.0700
0.0700
0.0703
0.0707
0.0710
0.0712
0.0712
0.0713
0.0716
0.0720
0.0723
0.0724
0.0727
0.0735
0.0740
0.0744
0.0780
0.0781
0.0786
0.0810
0.8
1.0
0.9
0.8
1.1
1.7
1.1
4.5
2.4
1.6
1.8
1.5
1.6
5.4
1.2
0.9
0.9
0.8
2.6
3.0
2.0
1.0
2.0
2.8
0.9
3.9
2.3
1.0
3.3
1.0
4.8
0.8
2.0
1.0
1.3
1.1
2.5
1.7
2.3
1.2
2.1
2.7
0.9
2.2
1.0
1.6
1.4
1.4
1.9
1.7
1.3
1.7
0.44
0.53
0.86
0.55
0.42
0.38
0.43
0.72
0.75
0.40
0.58
0.15
0.16
0.67
0.52
0.72
0.16
0.47
0.38
0.25
0.67
0.61
0.47
0.21
0.19
0.38
0.67
0.54
0.57
0.35
0.66
0.23
0.26
0.72
0.24
0.34
0.87
0.68
0.59
0.92
0.93
0.61
0.29
0.74
0.37
0.65
0.26
0.30
0.65
0.48
0.62
0.50
408.7
409.4
409.5
409.7
415.6
416.8
417.9
419.5
421.4
422.1
422.4
422.8
422.9
423.1
423.3
423.5
423.5
423.9
424.5
426.5
426.6
426.6
427.4
427.7
427.9
428.9
429.1
430.0
431.9
432.1
434.0
435.0
436.2
436.4
438.2
440.1
442.0
443.5
443.5
444.1
445.6
447.9
450.1
450.8
452.6
457.1
460.0
462.6
484.3
484.5
487.7
502.0
3.1
3.9
3.5
3.3
4.6
6.7
4.4
18.1
9.7
6.6
7.4
6.0
6.5
22.1
4.8
3.5
3.9
3.4
10.6
12.5
8.3
4.1
8.2
11.8
3.6
16.2
9.6
4.2
13.6
4.2
20.1
3.2
8.6
4.2
5.6
4.6
10.9
7.3
9.9
5.3
9.1
11.6
4.0
9.4
4.3
7.2
6.1
6.1
8.8
7.8
6.1
8.1
410.8
407.3
413.1
409.1
421.5
419.3
414.4
430.0
427.4
434.7
422.9
414.0
437.2
439.4
427.5
430.6
427.3
422.0
423.5
440.1
427.5
420.6
431.2
403.6
426.5
428.1
438.9
434.3
436.1
437.6
440.3
438.8
431.0
437.6
427.0
439.9
445.0
445.7
436.6
446.0
457.1
449.8
449.3
452.8
455.2
466.9
468.1
448.3
478.8
494.1
486.2
504.2
5.9
6.2
3.5
5.0
9.4
15.2
8.6
21.6
11.1
14.4
10.8
32.0
36.1
29.0
7.9
4.2
20.4
6.1
23.6
42.8
10.5
5.5
14.8
45.9
16.4
36.2
12.3
6.7
20.2
10.2
26.1
12.1
27.9
4.9
19.2
11.4
10.6
9.0
13.9
4.9
8.4
15.8
11.5
10.7
9.6
9.3
20.1
16.5
11.1
13.4
8.1
13.3
423.2
395.2
433.3
406.0
453.8
433.1
395.3
486.6
460.1
501.7
425.7
364.9
513.6
525.5
450.5
468.9
448.0
411.7
418.0
512.2
432.3
387.7
451.5
268.2
418.9
424.1
490.8
457.0
458.2
467.0
473.3
458.8
403.2
443.9
366.8
438.6
460.5
457.4
400.4
456.0
515.8
459.4
445.2
463.3
468.5
515.8
507.8
375.5
453.0
538.6
479.0
514.5
35.1
35.1
11.7
28.0
54.7
91.2
51.0
94.1
46.6
82.1
57.1
210.0
221.1
133.0
42.6
18.1
128.3
35.0
140.9
255.0
49.7
28.4
82.9
310.6
103.1
214.6
56.5
35.6
103.8
59.4
122.3
73.6
172.0
21.2
120.3
66.9
32.5
40.3
70.7
11.8
18.7
76.2
67.3
43.8
53.8
41.4
114.2
97.9
49.4
65.6
36.3
63.3
0.0815
0.0815
0.0818
0.0833
0.0855
0.0887
0.0899
0.0914
0.0927
0.0940
0.1421
0.1660
0.1921
0.1891
0.1989
0.1971
0.2322
0.2507
0.2596
0.2755
0.2940
0.3060
0.3090
0.3195
0.3071
0.3690
0.4113
0.9
1.7
3.3
1.6
5.3
1.5
2.9
4.2
2.3
3.0
4.4
0.7
1.6
1.3
1.2
1.6
1.6
1.4
1.3
2.6
2.4
1.3
0.8
0.6
2.0
3.1
1.5
0.49
0.16
0.38
0.24
0.70
0.79
0.15
0.83
0.61
0.89
0.97
0.92
0.75
0.27
0.79
0.54
0.69
0.86
0.66
0.37
0.49
0.75
0.62
0.96
0.99
0.81
0.97
505.0
505.2
506.7
515.9
528.6
548.1
555.0
563.8
571.4
579.2
856.4
990.0
1132.7
1116.7
1169.6
1159.8
1346.2
1441.9
1488.0
1568.7
1661.6
1720.9
1735.6
1787.5
1726.2
2024.5
2220.8
4.4
8.3
16.2
8.0
26.7
7.7
15.4
22.6
12.8
16.7
35.2
6.9
16.1
12.9
12.9
17.1
19.7
18.2
17.1
36.4
34.8
20.4
11.9
9.6
31.0
53.3
28.4
511.5
499.5
504.6
530.1
557.0
553.1
520.0
574.1
582.3
585.3
866.6
1003.2
1136.7
1129.4
1170.2
1165.7
1350.9
1448.6
1505.0
1622.4
1678.7
1720.3
1732.1
1827.5
1795.8
2099.1
2322.2
7.5
42.1
34.5
28.5
32.1
8.0
78.1
22.2
17.0
15.1
26.4
5.2
14.2
32.4
10.5
20.7
17.4
12.7
15.2
56.6
40.2
14.9
10.4
5.4
17.4
33.6
14.2
540.8
473.1
495.3
591.6
674.6
573.6
368.8
615.1
624.9
608.9
892.7
1032.2
1144.4
1153.8
1171.5
1176.8
1358.3
1458.3
1528.9
1692.8
1700.1
1719.7
1727.8
1873.3
1877.5
2173.0
2412.5
35.6
233.4
176.9
145.4
113.9
25.1
430.2
61.2
65.6
34.0
22.5
6.3
27.2
90.9
18.4
49.8
32.3
16.2
27.3
119.6
78.9
21.8
18.0
3.1
5.6
38.8
6.7
9312)
0.0256
0.0318
0.0363
0.0524
0.0540
0.0553
0.0621
0.0728
0.0800
0.1797
0.0819
0.0743
0.2486
0.2700
0.2861
0.2593
0.2838
0.2523
0.2669
0.2838
0.3071
0.2956
0.2761
5.2
7.9
9.0
6.5
3.8
8.6
2.8
5.7
2.8
2.4
3.3
8.6
1.5
9.3
4.9
3.5
4.9
3.8
2.4
6.1
2.8
1.3
2.9
0.58
0.85
0.87
0.94
0.90
0.99
0.96
0.88
0.72
0.84
0.80
0.97
0.97
1.00
0.98
0.97
0.99
0.99
0.99
1.00
0.97
0.94
0.97
163.1
202.1
229.7
329.1
339.3
346.9
388.5
452.7
495.9
1065.5
507.6
462.1
1431.5
1540.6
1622.2
1486.3
1610.6
1450.4
1525.2
1610.7
1726.5
1669.6
1571.7
8.4
15.8
20.2
20.7
12.7
29.1
10.6
24.8
13.3
23.2
16.2
38.3
19.0
127.2
69.8
46.8
70.5
49.4
33.2
86.3
42.4
19.3
40.4
173.0
213.7
386.4
431.8
458.2
492.5
510.0
600.8
632.9
1069.7
685.4
664.4
1559.1
1627.7
1676.2
1599.7
1680.1
1584.6
1630.1
1681.2
1747.0
1716.5
1682.2
14.3
18.0
33.2
24.3
15.8
34.1
11.7
29.3
18.2
18.5
20.8
43.1
12.2
75.6
40.6
29.2
41.0
30.7
20.0
49.9
24.1
11.5
24.6
310.5
343.0
1479.8
1024.6
1109.5
1242.7
1099.5
1208.1
1158.5
1078.2
1323.3
1429.0
1736.5
1742.2
1744.6
1752.4
1767.8
1768.2
1768.3
1770.3
1771.6
1774.2
1822.8
168.0
111.5
97.8
49.5
38.1
29.2
15.8
61.3
52.7
30.4
48.9
39.8
7.1
10.3
16.2
15.3
11.1
7.3
5.7
6.0
13.3
8.7
13.4
0.2702
0.3048
0.3430
0.2988
0.3007
0.3233
0.3234
0.2948
0.2998
0.2710
0.2893
0.3182
0.3285
0.3632
0.3618
0.0754
0.4178
0.3979
0.4264
0.4303
0.4608
0.3960
0.4834
0.4347
0.4719
6322, 133.74052)
0.0498
0.0514
0.0522
0.0535
0.0537
0.0540
0.0542
0.0547
0.0548
0.0548
0.0550
0.0550
0.0550
0.0550
0.0550
0.0551
0.0552
0.0552
0.0552
0.0552
0.0552
0.0552
0.0552
0.0553
0.0553
4.7
2.0
8.1
1.3
2.8
1.0
0.8
1.8
4.0
9.0
6.8
2.2
1.8
3.7
1.7
6.3
2.7
1.5
2.2
1.1
1.3
4.9
3.4
3.2
7.3
1.00
0.82
1.00
0.94
0.97
0.69
0.67
0.97
1.00
1.00
0.99
0.95
0.96
0.99
0.97
0.97
0.99
0.98
0.99
0.96
0.86
1.00
0.99
0.98
0.91
1541.8
1714.9
1901.0
1685.1
1694.7
1805.8
1806.2
1665.3
1690.5
1545.9
1638.1
1780.8
1830.9
1997.5
1990.5
468.8
2250.3
2159.3
2289.7
2307.3
2443.0
2150.5
2542.1
2327.0
2491.7
64.5
30.8
133.9
19.0
41.2
16.2
12.8
25.8
60.2
124.1
98.2
34.8
29.4
64.1
28.5
28.3
51.3
27.8
42.0
21.2
25.6
89.3
70.6
61.7
150.7
1665.7
1768.9
1871.4
1755.0
1766.7
1828.7
1829.5
1753.4
1774.7
1690.7
1764.9
1861.0
1944.1
2057.3
2066.3
896.2
2342.0
2334.3
2414.6
2441.8
2532.8
2422.9
2614.0
2518.2
2595.1
38.6
20.8
69.9
11.4
24.0
12.6
10.3
15.1
34.1
74.8
57.1
20.1
16.6
33.2
15.1
38.3
25.0
14.1
20.3
10.6
13.7
45.1
31.7
29.9
75.2
1825.6
1833.2
1838.7
1839.2
1852.9
1854.7
1856.1
1860.1
1875.1
1875.3
1918.5
1951.9
2067.0
2117.9
2142.7
2180.5
2422.9
2491.1
2521.6
2555.8
2605.6
2660.4
2670.2
2676.1
2676.9
5.6
25.7
12.6
8.4
13.2
19.5
16.4
7.9
6.6
15.1
12.6
13.2
9.3
9.2
6.8
26.8
7.5
5.3
5.6
5.6
12.5
5.1
6.0
9.8
54.9
2.8
5.2
2.3
9.5
1.0
5.0
1.8
4.5
1.7
2.0
1.5
3.1
1.0
2.0
1.6
1.0
1.5
0.9
1.4
1.0
0.9
1.5
2.1
3.1
1.0
0.91
0.90
0.89
0.95
0.37
0.97
0.46
0.81
0.77
0.78
0.45
0.49
0.56
0.52
0.23
0.33
0.64
0.31
0.75
0.43
0.36
0.50
0.69
0.88
0.26
313.6
322.9
328.3
336.0
337.4
338.8
340.2
343.6
343.9
344.2
345.0
345.1
345.1
345.2
345.4
345.8
346.1
346.1
346.2
346.4
346.5
346.6
346.6
346.9
346.9
8.6
16.3
7.5
31.1
3.3
16.5
6.0
14.9
5.9
6.6
4.9
10.4
3.3
6.7
5.4
3.4
5.0
2.9
4.7
3.3
3.1
5.0
7.1
10.5
3.5
318.8
330.1
333.9
335.0
338.8
340.4
339.8
348.7
342.6
339.2
345.1
345.4
347.5
342.5
341.1
349.4
347.1
350.9
345.6
347.8
349.0
346.7
352.7
351.9
355.8
8.5
16.2
7.4
28.6
7.7
14.9
11.4
16.3
6.6
7.3
9.5
18.6
5.2
11.1
19.7
8.9
6.8
8.1
5.4
6.6
7.5
8.7
9.1
10.4
12.2
357.0
381.4
373.2
327.6
348.3
351.4
337.0
383.0
333.6
305.6
346.3
347.2
363.3
323.7
311.8
373.5
354.0
382.1
341.0
356.9
366.0
347.4
392.5
384.9
414.4
29.4
55.9
26.5
72.7
55.7
28.5
79.5
73.3
33.1
36.1
65.4
125.3
33.2
74.1
150.7
63.9
39.7
58.0
27.4
45.9
53.6
57.9
49.2
37.0
87.6
0.0553
0.0553
0.0553
0.0554
0.0554
0.0554
0.0554
0.0554
0.0554
0.0555
0.0555
0.0555
0.0555
0.0555
0.0556
0.0556
0.0556
0.0556
0.0556
0.0557
0.0557
0.0557
0.0558
0.0558
0.0558
0.0558
0.0558
0.0558
0.0558
0.0559
0.0559
0.0559
0.0559
0.0559
0.0559
0.0559
0.0560
0.0560
0.0560
0.0561
0.0561
0.0561
0.0562
0.0562
0.0562
0.0562
0.0562
0.0563
0.0564
0.0564
0.0564
0.0565
2.8
1.5
1.1
0.9
4.3
1.2
1.0
1.4
2.1
1.2
3.1
1.7
2.9
2.4
1.0
1.2
1.4
0.6
1.0
0.9
0.9
1.0
1.2
1.1
1.7
1.0
1.6
1.4
1.1
0.9
1.3
2.5
1.3
3.8
0.9
1.5
2.5
1.0
1.3
0.9
1.1
0.9
1.6
0.9
1.1
1.3
2.3
1.2
1.4
1.5
3.3
1.1
0.80
0.31
0.47
0.40
0.76
0.18
0.39
0.52
0.55
0.33
0.75
0.39
0.77
0.83
0.41
0.65
0.19
0.28
0.28
0.22
0.40
0.30
0.17
0.21
0.32
0.45
0.54
0.51
0.38
0.28
0.42
0.69
0.43
0.73
0.24
0.46
0.44
0.34
0.56
0.38
0.18
0.64
0.36
0.34
0.36
0.72
0.80
0.52
0.22
0.47
0.65
0.25
347.0
347.2
347.2
347.5
347.6
347.7
347.7
347.7
347.8
348.0
348.1
348.2
348.2
348.4
348.8
348.9
348.9
348.9
349.0
349.1
349.6
349.7
349.9
350.0
350.1
350.1
350.1
350.3
350.3
350.4
350.4
350.7
350.7
350.9
350.9
350.9
351.2
351.4
351.5
351.8
352.0
352.2
352.4
352.5
352.5
352.5
352.7
352.8
353.5
353.7
353.9
354.3
9.4
5.2
3.6
3.1
14.4
4.1
3.4
4.7
7.1
3.9
10.4
5.9
9.7
8.3
3.6
4.1
4.7
2.2
3.4
3.1
3.2
3.5
3.9
3.6
5.8
3.3
5.6
4.6
3.9
3.2
4.3
8.4
4.4
13.0
3.0
5.1
8.5
3.4
4.4
3.2
3.6
3.1
5.3
3.3
3.7
4.6
7.8
4.0
4.8
5.2
11.3
3.9
342.3
343.6
347.7
341.4
346.3
339.3
345.9
341.5
346.7
350.0
347.4
349.6
347.3
351.5
348.2
351.2
361.2
348.1
349.5
350.6
345.2
350.9
356.8
338.5
348.9
351.0
356.9
352.7
348.5
341.7
346.9
355.1
348.4
359.5
356.8
352.5
351.8
347.1
352.8
351.2
341.3
354.0
345.0
345.2
345.4
354.0
352.8
354.6
354.7
358.8
361.2
349.9
10.1
14.5
6.7
6.8
16.4
19.0
7.6
7.8
11.3
10.3
12.1
13.2
11.0
8.7
7.5
5.5
22.2
6.7
10.6
12.7
7.0
10.0
20.0
15.0
15.8
6.5
9.1
8.0
8.7
9.8
9.0
10.6
8.9
15.8
11.0
9.6
16.7
8.6
6.8
7.3
16.7
4.3
12.6
8.3
8.8
5.6
8.5
6.7
19.2
9.6
15.4
13.5
310.8
319.3
351.0
300.2
337.6
282.5
334.2
299.3
339.0
363.3
343.2
359.1
341.4
371.9
343.8
366.5
440.7
342.5
352.5
360.4
315.4
359.0
402.0
260.3
341.4
357.0
401.1
368.5
336.5
282.7
323.3
383.9
332.8
415.0
395.3
362.9
355.8
318.1
360.9
347.1
268.6
366.1
295.3
296.4
298.2
363.7
353.1
365.7
362.0
392.0
408.7
321.0
48.1
107.2
45.3
49.1
82.5
148.1
54.3
52.0
72.6
74.1
62.1
92.5
54.0
36.7
52.2
32.0
159.9
49.0
77.9
94.7
49.6
72.6
146.6
117.0
115.3
44.0
57.0
51.9
61.9
74.1
63.0
57.6
62.0
79.7
79.9
64.1
113.5
62.7
42.8
51.2
130.1
25.1
91.4
60.8
63.7
29.2
38.0
42.7
141.1
62.5
86.3
100.2
0.0565
0.0566
0.0566
0.0566
0.0566
0.0566
0.0567
0.0567
0.0568
0.0568
0.0568
0.0571
0.0571
0.0575
0.0617
0.2233
0.2939
0.2706
0.3276
0.3484
0.3601
0.5353
4790, 133.72441)
0.0546
0.0548
0.0549
0.0550
0.0551
0.0552
0.0554
0.0554
0.0555
0.0555
0.0556
0.0556
0.0557
0.0557
0.0558
0.0559
0.0559
0.0561
0.0561
0.0562
0.0564
0.0564
0.0565
0.0565
0.0567
0.0568
0.0569
0.0570
5.7
1.7
2.4
1.0
0.9
3.3
3.6
0.9
5.0
1.5
1.2
2.3
0.8
1.7
8.7
1.8
2.1
5.4
1.6
0.8
1.2
0.8
0.92
0.39
0.48
0.36
0.23
0.72
0.85
0.48
0.91
0.25
0.31
0.50
0.83
0.54
0.94
0.99
0.98
1.00
0.73
0.80
0.69
0.89
354.4
354.8
354.8
354.9
355.0
355.0
355.3
355.8
356.0
356.0
356.1
357.8
357.8
360.3
385.8
1299.1
1661.0
1544.1
1826.9
1926.7
1982.9
2763.6
19.8
6.0
8.4
3.6
3.2
11.5
12.5
3.3
17.2
5.1
4.1
7.9
2.8
5.8
32.5
20.8
30.1
73.7
24.8
13.9
20.9
18.5
356.9
360.3
352.4
354.6
354.9
348.8
352.7
354.8
355.7
356.2
348.0
367.7
358.4
355.6
379.5
1313.4
1656.2
1643.2
1830.0
1927.1
2102.0
2752.8
18.9
13.6
15.3
8.6
12.4
13.8
12.6
5.9
16.4
17.6
11.5
13.9
2.9
9.3
29.4
13.2
17.2
43.7
18.2
9.0
15.9
8.7
372.7
396.1
337.1
352.5
354.3
307.6
335.6
348.8
353.6
357.3
294.2
430.9
361.9
324.8
341.5
1336.7
1650.2
1772.4
1833.5
1927.4
2220.6
2744.8
56.8
93.1
102.2
60.5
90.8
73.9
50.2
39.3
51.4
128.3
84.9
86.9
12.3
59.2
74.0
5.4
8.3
4.5
26.7
11.1
22.6
6.9
1.8
0.8
0.8
2.4
3.7
1.3
1.5
1.5
1.4
1.4
1.1
0.9
0.7
1.0
4.4
2.5
2.4
1.1
1.0
0.8
2.2
1.9
4.3
1.1
1.0
1.6
1.3
1.5
0.62
0.18
0.54
0.31
0.61
0.72
0.16
0.27
0.73
0.40
0.24
0.59
0.23
0.40
0.67
0.83
0.51
0.50
0.21
0.51
0.67
0.42
0.85
0.57
0.54
0.78
0.39
0.66
342.6
344.1
344.8
345.2
345.8
346.2
347.3
347.5
347.9
348.3
348.8
348.9
349.3
349.3
350.2
350.6
350.8
352.0
352.0
352.6
353.4
353.9
354.3
354.3
355.4
356.3
356.7
357.4
5.9
2.6
2.8
8.0
12.3
4.3
5.0
5.1
4.8
4.7
3.9
3.0
2.5
3.5
15.2
8.6
8.1
3.6
3.4
2.6
7.5
6.5
14.8
3.8
3.5
5.7
4.5
5.1
345.4
338.3
346.8
364.4
344.1
347.9
353.7
355.3
347.9
347.8
338.7
346.5
350.2
351.2
349.6
353.9
349.3
351.9
355.1
352.2
357.4
350.4
352.1
355.0
352.6
353.0
358.0
357.7
8.4
11.9
4.5
23.6
17.5
5.2
27.6
16.7
5.7
10.2
14.0
4.4
9.7
7.7
19.7
9.1
13.9
6.3
13.8
4.4
9.8
13.2
15.1
5.8
5.6
6.3
10.2
6.7
364.1
298.1
360.3
488.4
332.4
359.6
396.0
406.9
347.8
344.2
270.3
330.7
356.4
363.7
346.1
375.9
339.2
351.5
375.5
349.2
383.6
327.4
337.9
359.1
334.3
331.5
366.7
359.3
51.1
92.9
29.3
162.0
107.2
27.5
204.8
119.9
30.0
71.7
108.0
27.6
71.9
53.4
111.9
37.9
91.7
41.4
101.0
28.8
54.5
91.7
61.4
35.7
36.0
30.2
70.2
37.9
0.0571
0.0571
0.0577
0.0578
0.0580
0.0580
0.0581
0.0589
0.0686
0.0690
0.1066
0.1797
0.1794
0.1950
0.1993
0.2202
0.2292
0.2217
0.2396
0.2864
0.2783
0.2760
0.2852
0.3122
0.3208
0.3142
0.3129
0.3218
0.3163
0.3012
0.3124
0.3244
0.3340
0.3315
0.3390
0.3385
0.3344
0.3300
0.3262
0.3266
0.3217
0.3283
0.3459
0.3297
0.3276
0.3455
0.3448
0.3452
0.3458
0.3437
0.3469
0.3652
2.1
1.9
1.3
0.9
3.3
1.0
2.8
2.9
2.6
1.7
1.2
1.5
1.1
2.1
2.1
2.3
2.0
3.5
1.6
1.1
2.1
2.2
1.7
2.0
1.0
0.7
1.3
0.9
1.1
0.8
1.7
1.3
2.4
1.0
1.8
2.3
1.1
1.6
2.3
2.7
1.6
2.3
1.4
1.1
2.7
2.4
1.4
1.3
1.6
1.5
1.1
1.1
0.54
0.53
0.38
0.18
0.96
0.81
0.20
0.90
0.38
0.21
0.82
0.67
0.68
0.72
0.49
0.41
0.95
0.99
0.68
0.81
0.98
0.88
0.72
0.74
0.66
0.71
0.94
0.88
0.90
0.98
0.92
0.87
0.95
0.54
0.90
0.99
0.98
0.75
0.88
0.90
0.95
0.89
0.75
0.86
0.72
0.66
0.33
0.90
0.95
0.97
0.44
0.93
357.7
357.9
361.4
362.3
363.2
363.6
364.2
368.7
427.7
430.0
653.0
1065.3
1063.5
1148.4
1171.5
1283.1
1330.4
1290.7
1384.5
1623.5
1582.6
1571.0
1617.3
1751.6
1793.5
1761.2
1755.2
1798.5
1771.6
1697.3
1752.5
1811.0
1857.6
1845.6
1882.0
1879.4
1859.6
1838.2
1820.0
1821.8
1798.1
1829.9
1915.0
1836.8
1826.8
1913.1
1909.9
1911.7
1914.6
1904.4
1919.9
2006.9
7.2
6.6
4.5
3.0
11.6
3.6
9.9
10.2
10.6
6.9
7.7
14.8
10.7
21.6
22.2
26.6
23.5
40.4
19.4
15.1
30.0
30.9
24.7
30.9
15.1
11.0
19.6
13.6
17.3
11.7
25.4
21.0
39.2
15.5
29.1
37.4
17.8
25.4
37.2
43.3
24.4
36.4
23.8
17.9
42.8
39.0
22.7
22.3
27.0
25.1
18.4
19.1
368.5
361.9
363.4
358.5
364.0
365.8
337.7
366.1
415.6
416.7
661.1
1072.5
1073.6
1148.9
1170.5
1270.4
1329.6
1314.8
1387.5
1627.1
1604.3
1602.7
1638.6
1745.9
1784.7
1767.5
1768.1
1792.4
1777.9
1741.0
1778.9
1817.3
1845.7
1840.9
1861.4
1861.2
1851.2
1841.2
1833.4
1836.9
1825.6
1844.3
1891.7
1854.8
1851.3
1902.6
1904.3
1913.3
1921.0
1917.5
1927.5
1997.9
11.7
10.9
10.1
14.1
10.5
3.8
40.0
9.7
23.1
26.6
7.3
14.8
10.7
19.6
29.3
40.4
15.3
25.8
17.4
10.6
17.7
20.3
19.5
22.9
12.2
8.4
11.3
8.2
10.4
6.7
15.1
12.9
21.7
15.0
16.9
19.8
9.6
18.1
22.6
25.7
13.9
21.8
16.4
11.1
31.8
30.4
35.6
12.9
14.9
13.5
21.5
10.4
437.1
387.7
376.3
333.9
369.1
379.5
159.0
349.6
349.0
343.6
688.9
1087.4
1094.2
1149.8
1168.7
1248.8
1328.3
1354.4
1392.1
1631.7
1633.0
1644.6
1666.0
1739.1
1774.5
1774.9
1783.4
1785.3
1785.4
1793.9
1810.1
1824.6
1832.3
1835.6
1838.5
1840.8
1841.6
1844.6
1848.7
1854.1
1857.1
1860.5
1866.2
1875.1
1879.0
1891.2
1898.1
1915.0
1928.0
1931.8
1935.7
1988.7
70.5
67.8
69.1
104.2
23.0
16.3
320.2
31.4
141.5
172.6
18.3
33.3
23.8
39.0
72.8
99.4
13.1
10.5
32.5
14.3
8.8
22.5
30.7
34.1
19.7
13.0
8.2
8.3
9.7
2.7
13.0
13.4
14.1
26.9
15.7
5.9
4.3
25.6
22.9
23.5
9.3
21.1
22.7
12.0
46.6
47.6
70.2
11.5
10.1
6.9
39.9
8.1
0.3598
0.3619
0.3852
0.4008
0.4144
0.4357
0.4365
0.4134
0.4438
0.3890
0.4707
0.4902
0.4978
0.4935
0.4886
0.5065
0.5222
0.5264
0.5801
0.5999
0.5928
0.5877
0.5823
0.5957
0.6381
1.3
2.1
0.8
1.6
2.8
0.9
2.3
4.5
2.6
6.7
0.8
2.0
4.4
1.4
1.3
1.7
2.7
1.5
0.9
0.9
0.9
3.6
2.6
0.8
1.8
0.90
0.68
0.29
0.76
0.81
0.97
0.98
0.91
0.99
1.00
0.53
0.87
0.99
0.86
0.96
0.96
0.97
0.94
0.99
0.99
1.00
1.00
0.98
0.99
0.98
1981.2
1991.1
2100.5
2172.9
2234.8
2331.4
2334.9
2230.6
2367.5
2118.2
2486.5
2571.6
2604.3
2585.8
2564.6
2641.6
2708.6
2726.1
2949.2
3029.6
3000.9
2980.0
2958.0
3012.4
3181.7
22.4
35.9
13.6
29.7
53.4
18.1
46.0
85.8
52.2
121.8
17.4
43.3
93.5
28.8
28.0
37.1
60.5
32.6
20.4
20.8
20.5
85.1
62.7
19.1
45.9
1989.2
1995.2
2088.3
2169.0
2238.6
2327.4
2337.6
2309.7
2384.1
2310.1
2485.8
2587.0
2602.1
2598.9
2625.3
2671.4
2718.4
2749.2
2960.1
2992.7
2981.4
2973.0
2964.2
2986.3
3213.1
12.7
26.9
23.5
19.1
31.6
8.7
22.0
45.4
24.4
61.6
14.8
21.9
41.2
14.7
12.9
16.8
26.6
14.8
8.4
8.4
8.3
34.4
25.8
7.7
18.2
1997.4
1999.4
2076.4
2165.3
2242.1
2323.9
2340.1
2380.3
2398.4
2484.4
2485.2
2599.1
2600.3
2609.2
2672.5
2694.0
2725.7
2766.2
2967.5
2968.0
2968.3
2968.3
2968.3
2968.8
3232.8
11.1
40.0
44.8
24.3
35.5
4.3
8.7
34.6
6.1
4.4
22.8
19.2
8.2
13.3
6.1
8.4
10.6
8.7
2.1
2.1
1.1
4.9
7.6
2.0
6.4
33.77415)
0.0082
0.0083
0.0084
0.0084
0.0085
0.0085
0.0086
0.0086
0.0087
0.0088
0.0092
0.0092
0.0094
0.0103
0.0106
0.0108
0.0109
0.0109
0.0112
0.0155
0.0165
0.0188
0.0239
0.0242
0.0337
1.7
0.8
1.2
1.0
2.6
1.6
1.9
1.0
2.8
1.8
1.2
1.6
5.3
3.1
1.6
1.8
0.7
1.3
0.9
1.7
1.4
7.4
1.7
0.2
1.8
0.41
0.21
0.35
0.65
0.88
0.74
0.85
0.40
0.89
0.75
0.59
0.72
0.98
0.92
0.70
0.65
0.37
0.75
0.81
0.75
0.71
1.00
0.66
0.25
0.64
52.9
53.3
53.8
54.2
54.4
54.8
55.4
55.5
56.1
56.6
59.0
59.2
60.3
65.9
67.8
69.0
69.9
70.0
71.7
99.4
105.3
119.8
152.1
154.1
213.4
0.9
0.4
0.6
0.5
1.4
0.9
1.1
0.5
1.5
1.0
0.7
1.0
3.2
2.0
1.1
1.2
0.5
0.9
0.7
1.6
1.4
8.7
2.5
0.4
3.7
53.5
53.7
56.1
53.5
53.9
55.3
54.3
55.4
55.7
56.4
59.1
68.2
60.7
67.0
68.7
69.8
70.2
69.7
71.4
99.1
103.8
120.4
153.5
152.8
211.3
2.1
2.0
1.8
0.8
1.6
1.1
1.2
1.3
1.7
1.4
1.1
1.5
3.2
2.2
1.5
1.8
1.2
1.1
0.8
2.1
1.9
8.4
3.6
1.4
5.3
80.7
70.6
157.3
25.1
32.2
78.2
5.3
52.1
39.2
48.5
62.8
398.3
74.2
105.4
96.7
99.0
78.5
57.4
60.1
90.3
69.4
132.0
176.0
133.7
188.7
87.6
90.9
71.8
27.6
34.0
34.0
28.5
53.3
34.2
39.4
38.2
34.7
27.2
30.5
39.7
49.2
40.5
26.9
15.8
34.7
32.1
13.1
44.8
22.4
49.9
0.0350
0.0486
0.0506
0.0519
0.0528
0.0532
0.0536
0.0554
0.0557
0.0560
0.0560
0.0560
0.0561
0.0564
0.0565
0.0568
0.0568
0.0570
0.0571
0.0573
0.0574
0.0574
0.0574
0.0577
0.0578
0.0578
0.0580
0.0580
0.0582
0.0582
0.0583
0.0583
0.0585
0.0585
0.0586
0.0587
0.0587
0.0587
0.0589
0.0589
0.0589
0.0589
0.0589
0.0589
0.0590
0.0591
0.0591
0.0592
0.0593
0.0593
0.0593
0.0593
1.9
1.5
0.7
4.0
5.7
3.6
1.4
2.6
1.4
3.1
1.4
0.9
1.2
0.6
3.5
2.3
0.6
2.0
2.7
1.2
2.0
1.1
3.2
2.3
1.5
1.9
0.5
1.9
2.6
1.1
1.5
0.8
1.6
2.1
2.6
0.9
0.8
1.3
1.3
5.3
2.1
1.5
1.0
4.1
1.5
2.6
0.9
1.8
0.9
1.5
2.2
2.0
0.70
0.90
0.63
0.99
0.99
0.97
0.81
0.96
0.93
0.96
0.89
0.67
0.92
0.51
0.98
0.93
0.58
0.79
0.95
0.84
0.96
0.89
0.96
0.96
0.91
0.81
0.65
0.94
0.95
0.78
0.89
0.72
0.89
0.91
0.97
0.85
0.76
0.93
0.81
0.98
0.97
0.89
0.78
0.98
0.90
0.84
0.81
0.85
0.81
0.79
0.89
0.95
221.7
305.7
318.1
326.2
331.9
334.1
336.8
347.5
349.3
351.0
351.3
351.4
351.7
353.5
354.4
355.9
356.1
357.4
358.2
358.9
359.6
359.9
360.1
361.6
362.0
362.4
363.4
363.6
364.4
364.7
365.2
365.5
366.5
366.6
367.2
367.4
367.9
367.9
368.9
368.9
369.0
369.1
369.2
369.2
369.7
370.0
370.2
370.7
371.5
371.5
371.5
371.7
4.2
4.6
2.3
12.7
18.6
11.9
4.6
8.9
4.8
10.5
4.6
3.1
3.9
2.0
12.2
7.9
2.2
7.0
9.5
4.1
6.9
4.0
11.3
8.1
5.3
6.7
1.7
6.6
9.2
3.8
5.5
2.7
5.6
7.5
9.4
3.2
2.8
4.7
4.8
18.9
7.6
5.2
3.6
14.6
5.3
9.4
3.3
6.5
3.4
5.5
7.9
7.4
222.5
313.2
328.8
333.7
339.6
341.0
338.1
350.5
352.3
350.3
354.7
356.3
355.2
355.9
356.5
358.5
358.2
359.7
361.0
359.8
360.1
364.0
364.8
362.8
364.3
367.1
364.6
367.6
368.0
366.7
364.5
367.2
365.5
366.9
367.5
370.1
372.2
368.0
369.7
370.6
370.0
368.3
370.9
369.8
369.1
371.0
368.8
374.8
372.6
373.9
373.7
372.2
5.5
4.6
3.3
11.5
16.8
10.9
5.0
8.1
4.6
9.4
4.5
4.0
3.8
3.4
10.8
7.4
3.3
7.8
8.7
4.2
6.3
3.9
10.3
7.3
5.1
7.3
2.2
6.1
8.5
4.2
5.3
3.2
5.4
7.2
8.3
3.3
3.2
4.3
5.1
16.6
6.8
5.1
4.0
12.9
5.0
9.7
3.6
6.6
3.6
6.0
7.7
6.7
231.3
369.2
405.3
386.0
392.2
387.7
347.3
370.2
372.2
345.4
377.0
388.4
378.6
371.4
369.9
375.6
372.2
374.7
378.6
365.7
363.3
389.9
394.9
370.8
378.6
396.9
372.8
392.6
390.7
379.4
360.5
377.8
359.2
369.1
369.3
386.7
399.2
368.9
374.3
381.1
376.6
363.3
381.8
373.8
365.4
377.1
359.5
399.7
379.6
388.6
387.6
375.6
45.2
17.1
20.1
12.7
19.8
19.6
22.8
16.7
13.0
19.4
15.4
22.5
11.3
22.2
15.8
20.3
20.1
35.7
19.8
17.2
13.4
13.3
21.9
14.6
15.3
31.5
12.4
14.7
20.1
18.9
17.9
16.2
17.9
22.3
14.5
12.9
15.1
11.6
21.4
20.8
12.0
16.5
18.2
19.7
15.7
37.6
15.2
25.1
15.2
25.9
25.6
15.2
0.0594
0.0594
0.0594
0.0595
0.0595
0.0595
0.0595
0.0595
0.0596
0.0597
0.0597
0.0597
0.0598
0.0598
0.0598
0.0599
0.0600
0.0601
0.0602
0.0603
0.0604
0.0605
0.0605
0.0605
0.0606
0.0608
0.0608
0.0608
0.0608
0.0609
0.0609
0.0610
0.0610
0.0610
0.0610
0.0610
0.0611
0.0611
0.0611
0.0612
0.0612
0.0613
0.0614
0.0615
0.0616
0.0616
0.0617
0.0618
0.0618
0.0620
0.0620
0.0624
0.6
2.0
1.3
4.3
1.5
3.2
1.0
1.0
1.1
2.5
1.8
1.6
2.7
1.8
1.1
1.0
1.8
1.2
1.1
1.0
1.1
0.6
0.5
1.6
1.6
2.2
1.1
1.1
1.7
1.1
1.1
1.0
1.5
1.8
0.8
0.4
1.0
2.1
1.9
1.3
1.5
1.6
2.2
1.7
1.9
1.7
2.0
1.4
1.7
1.5
1.4
1.6
0.69
0.91
0.83
0.99
0.91
0.96
0.68
0.76
0.78
0.96
0.87
0.92
0.96
0.92
0.77
0.71
0.85
0.85
0.82
0.85
0.67
0.46
0.40
0.68
0.82
0.95
0.88
0.88
0.91
0.78
0.69
0.75
0.93
0.93
0.66
0.35
0.65
0.93
0.96
0.91
0.88
0.70
0.93
0.91
0.93
0.83
0.86
0.78
0.94
0.84
0.82
0.83
371.9
371.9
372.0
372.3
372.4
372.5
372.5
372.6
373.3
373.9
374.0
374.0
374.3
374.5
374.6
375.2
375.8
376.3
376.6
377.7
377.9
378.8
378.9
378.9
379.4
380.5
380.5
380.7
380.7
381.3
381.4
381.4
381.4
381.4
381.5
381.8
382.3
382.3
382.4
382.6
382.9
383.5
383.9
384.9
385.4
385.4
385.7
386.4
386.8
387.5
387.8
389.9
2.3
7.3
4.8
15.6
5.3
11.5
3.8
3.5
4.0
8.9
6.5
5.9
9.8
6.5
4.2
3.5
6.6
4.2
4.0
3.8
4.2
2.2
2.0
5.8
5.7
8.1
4.0
4.0
6.3
3.9
4.0
3.6
5.6
6.6
2.8
1.4
3.5
7.9
7.0
5.0
5.7
5.8
8.1
6.4
7.1
6.5
7.4
5.2
6.3
5.8
5.2
6.0
369.9
370.0
374.4
371.0
372.7
375.6
374.1
373.2
374.0
375.8
374.5
372.2
376.3
375.8
376.1
373.1
376.1
374.6
375.0
376.7
378.7
379.6
378.3
377.9
375.2
377.5
376.8
379.3
379.8
379.1
381.1
379.3
379.8
379.2
381.2
380.4
377.6
379.8
381.1
381.9
380.3
383.6
380.3
381.3
383.1
378.8
383.6
382.7
384.2
387.0
383.7
390.0
2.8
6.8
5.0
13.6
5.1
10.3
4.8
4.0
4.3
8.0
6.5
5.5
8.8
6.1
4.7
4.2
6.7
4.2
4.2
3.8
5.4
4.2
4.3
7.3
6.0
7.2
3.9
3.9
5.9
4.3
5.0
4.1
5.1
6.1
3.6
3.4
4.6
7.3
6.3
4.7
5.5
7.0
7.4
5.9
6.6
6.5
7.4
5.6
5.7
5.9
5.4
6.2
357.5
358.2
389.1
362.7
375.0
394.8
384.2
376.4
378.7
387.2
377.6
360.8
388.2
384.0
385.6
359.9
377.6
363.6
365.4
370.7
383.0
384.5
374.8
372.2
349.8
359.2
354.2
370.7
373.9
365.8
379.2
366.8
369.6
365.2
379.6
371.4
349.3
364.6
373.6
377.4
364.4
384.6
358.3
359.4
369.6
338.7
371.0
360.6
368.6
383.7
359.1
390.3
14.9
20.1
20.2
14.8
15.3
20.0
25.5
18.4
19.4
15.5
23.4
15.4
18.0
17.5
21.5
21.1
25.3
16.0
17.4
14.4
28.6
26.2
27.8
38.2
24.8
16.2
13.2
13.2
17.7
19.4
25.7
19.2
13.3
15.7
19.2
22.2
25.4
19.4
13.2
13.8
18.7
35.1
18.8
17.1
17.4
25.7
26.6
24.9
13.1
22.2
22.0
24.2
0.0624
0.0636
0.0638
0.0649
0.0649
0.1923
3.4
4.2
0.9
3.2
2.8
1.5
0.96
0.98
0.28
0.64
0.97
0.90
390.4
397.6
398.5
405.3
405.5
1133.6
12.9
16.3
3.3
12.4
11.2
15.4
386.4
396.8
399.7
413.5
397.7
1132.2
11.4
14.2
10.3
16.8
9.6
11.2
362.3
392.5
406.8
459.3
352.7
1129.3
23.2
19.5
66.9
84.5
16.1
14.1
77412)
0.0094
0.0095
0.0095
0.0096
0.0097
0.0100
0.0154
0.1686
0.1669
0.2282
0.2329
0.2766
0.0787
0.2897
0.3241
0.3230
0.3192
0.2608
0.3123
0.3137
0.3264
0.3283
0.3242
0.3190
0.2925
0.3151
0.2854
0.3184
0.3136
0.3156
0.3321
0.3220
0.3225
0.3286
0.3234
0.3311
0.3252
0.3308
0.3310
0.3289
0.3162
0.3096
0.3193
0.3269
3.2
5.7
2.8
3.3
2.9
9.8
3.1
2.6
2.8
1.1
2.8
0.9
4.2
2.9
1.5
0.9
1.3
6.5
3.5
0.8
1.7
2.3
3.9
1.2
1.3
1.0
1.4
2.8
1.7
0.8
2.2
1.3
1.0
1.1
0.6
1.8
1.4
1.3
0.9
1.9
1.3
1.0
2.6
1.4
0.23
0.36
0.09
0.07
0.38
0.32
0.25
0.97
0.83
0.21
0.90
0.73
0.97
0.99
0.71
0.65
0.89
0.94
0.78
0.75
0.62
0.86
0.96
0.85
0.93
0.57
0.40
0.80
0.97
0.68
0.68
0.89
0.71
0.78
0.23
0.84
0.63
0.58
0.62
0.64
0.74
0.78
0.79
0.96
60.0
60.8
61.2
61.3
62.4
63.9
98.2
1004.3
994.9
1325.2
1349.8
1574.1
488.6
1640.1
1809.7
1804.2
1785.8
1494.0
1752.1
1759.1
1821.0
1830.3
1810.3
1785.0
1654.0
1765.7
1618.5
1781.7
1758.5
1768.1
1848.6
1799.3
1802.0
1831.8
1806.4
1843.8
1815.3
1842.4
1843.1
1832.9
1770.9
1738.7
1786.5
1823.5
1.9
3.4
1.7
2.0
1.8
6.2
3.1
24.6
25.6
13.0
33.6
13.1
19.6
42.2
23.0
13.9
19.6
86.8
53.4
12.5
26.4
36.1
61.1
19.2
19.7
15.5
19.7
44.3
26.6
11.9
35.4
20.7
15.4
17.1
9.8
29.5
22.8
21.3
15.0
29.7
20.3
15.8
41.0
21.8
49.7
56.1
51.9
43.8
62.3
60.8
101.4
1018.4
1054.9
1310.8
1348.0
1608.4
762.4
1683.4
1803.1
1802.1
1795.9
1630.3
1781.7
1789.7
1824.1
1829.3
1819.0
1806.9
1734.3
1798.1
1715.8
1807.5
1795.9
1802.7
1846.3
1819.9
1821.4
1837.5
1824.4
1844.8
1829.6
1844.4
1845.0
1840.0
1806.6
1789.2
1816.7
1837.0
6.7
8.6
15.5
20.9
4.6
17.9
12.0
17.6
21.8
37.6
22.9
10.3
23.0
24.2
17.3
11.5
11.8
56.2
37.5
9.1
22.6
22.5
34.0
12.2
12.0
14.8
28.5
30.2
15.1
9.6
27.7
12.5
11.7
11.7
22.7
18.7
19.2
19.4
12.9
24.8
15.0
11.2
28.3
12.2
-423.9
-140.9
-358.7
-831.7
57.0
-60.0
177.1
1048.9
1181.4
1287.3
1345.3
1653.5
1679.8
1737.9
1795.4
1799.5
1807.6
1810.9
1816.5
1825.6
1827.6
1828.2
1829.0
1832.3
1832.5
1835.9
1836.6
1837.3
1839.6
1842.9
1843.6
1843.7
1843.8
1843.8
1845.0
1845.8
1846.0
1846.5
1847.2
1847.9
1848.0
1848.6
1851.6
1852.3
352.1
363.3
801.3
1462.1
167.5
712.9
281.5
14.5
36.2
97.1
25.8
16.2
17.6
7.7
26.3
18.9
11.6
42.5
50.7
13.0
37.7
24.9
19.7
13.6
9.4
26.0
57.2
39.1
8.5
15.1
43.3
12.2
17.7
15.6
47.3
21.9
31.7
33.6
21.7
40.6
21.6
15.0
37.5
7.4
0.3152
0.3195
0.3449
0.3272
0.3289
0.3290
0.3312
0.3308
0.3271
0.3051
0.3136
0.3397
0.3435
0.3406
0.3472
0.3010
0.3436
0.3428
0.3421
0.3288
0.3355
0.3440
0.3078
0.3091
0.3295
0.3105
0.3390
0.3439
0.3291
0.3435
0.3739
0.3698
0.3612
0.3660
0.3540
0.4074
0.4367
0.4661
0.4696
0.4773
0.4450
0.5091
0.5182
0.5087
0.5253
1.6
1.1
2.8
1.5
1.2
1.1
1.5
2.6
1.4
1.7
1.0
0.5
1.2
1.6
1.5
1.7
1.0
2.8
2.0
3.2
2.7
1.1
1.1
1.4
1.2
1.6
1.1
1.5
1.9
1.2
1.4
1.1
1.7
1.4
3.8
2.2
4.1
5.7
2.1
5.0
2.7
1.4
1.7
1.3
3.1
0.75
0.75
0.89
0.86
0.45
0.56
0.53
0.70
0.82
0.75
0.83
0.50
0.45
0.53
0.78
0.97
0.54
0.91
0.80
0.86
0.93
0.46
0.72
0.94
0.69
0.52
0.79
0.63
0.92
0.85
0.71
0.72
0.80
0.86
0.99
0.91
0.90
0.99
0.97
0.99
0.98
0.82
0.93
0.92
0.98
1766.3
1787.2
1910.3
1824.8
1833.2
1833.7
1844.4
1842.1
1824.2
1716.7
1758.5
1885.0
1903.7
1889.4
1921.3
1696.1
1903.8
1900.4
1896.6
1832.3
1864.7
1905.7
1730.1
1736.1
1835.9
1743.2
1881.7
1905.3
1834.2
1903.4
2047.9
2028.3
1987.7
2010.4
1953.6
2203.2
2336.0
2466.2
2481.7
2515.3
2373.1
2652.9
2691.7
2651.1
2721.6
24.6
17.2
46.8
23.4
19.1
17.0
24.1
42.4
22.9
25.0
15.9
8.3
19.6
26.0
25.5
25.1
16.1
46.7
32.9
51.5
43.8
18.4
17.0
21.1
19.1
24.4
17.5
24.2
30.1
20.2
23.7
19.9
29.2
24.6
64.6
40.5
81.1
116.4
43.7
104.2
53.9
31.2
37.1
28.0
67.7
1807.2
1818.8
1884.3
1839.3
1844.4
1845.4
1852.1
1851.0
1849.6
1795.1
1820.4
1889.2
1901.8
1894.6
1914.1
1793.0
1906.4
1905.6
1904.8
1872.2
1890.0
1911.9
1818.0
1824.2
1878.8
1829.3
1906.4
1920.3
1883.0
1977.4
2052.8
2049.2
2030.0
2045.1
2016.5
2267.3
2391.9
2508.8
2535.4
2567.8
2518.6
2674.5
2695.9
2684.6
2720.0
U age is <600 Ma.
m 206Pb/207Pb age for analyses with 206Pb/238Uage > 900 Ma.
8U ages <600 Ma because of large uncertainty in 206Pb/207Pb age
18.0
12.5
27.1
14.5
22.7
16.3
24.0
32.0
14.9
18.6
10.5
8.7
22.5
25.7
17.0
14.6
15.7
27.0
21.5
32.1
24.9
21.1
13.2
12.5
14.9
25.9
11.6
20.0
17.6
12.5
16.8
14.0
18.7
14.6
33.8
21.6
42.1
53.6
20.5
47.4
25.7
16.4
17.0
13.3
29.6
1854.8
1855.2
1855.7
1855.8
1857.0
1858.5
1860.8
1861.1
1878.2
1887.5
1891.9
1893.8
1899.7
1900.2
1906.3
1907.5
1909.3
1911.3
1913.7
1916.7
1917.8
1918.6
1920.3
1926.2
1926.5
1928.7
1933.4
1936.5
1937.3
2055.7
2057.6
2070.3
2073.2
2080.3
2081.5
2325.7
2439.8
2543.5
2578.7
2609.5
2638.1
2690.8
2699.0
2710.0
2718.9
25.6
17.7
25.6
15.7
43.2
28.8
43.1
48.1
18.0
26.2
12.4
15.8
41.9
45.6
22.4
7.7
27.6
23.9
26.8
34.6
19.1
39.1
19.4
8.9
22.7
46.6
14.8
32.1
14.5
13.2
23.6
19.4
22.4
14.9
8.0
16.8
33.3
16.2
9.3
13.4
8.5
16.3
10.6
9.4
11.2
included.
s that fall off of concordia are designated as "Discordant" in column "u" and are not considered further.
ned in the body of the manuscript)
are not included.
(206Pb/207Pb)] Actual values are reported in column "U" for each sample.
20%.
cey and Kramers (1975).
2.0 for 208Pb/204Pb.
f 563.5 ± 3.2 Ma (2-sigma).
38U/235U = 137.88.
ter routine)
try of Paleozoic and Triassic Passive Margin Strata of Western North America: Geosphere.
ution of U-Pb ages by laser ablation-multicollector-inductively coupled plasma mass spectrometry: Geoc
e model: Earth and Planetary Science Letters, v. 26, p. 207-221.
Best age
(Ma)
311.2
345.6
355.1
360.1
363.3
364.0
368.8
372.3
377.2
380.8
382.0
382.7
383.6
385.5
388.5
389.6
390.2
390.4
390.7
390.7
391.9
392.1
392.9
393.7
394.3
394.6
394.7
394.9
395.0
395.1
395.2
395.4
396.2
396.2
396.2
396.5
396.7
398.2
398.7
398.8
399.0
399.0
399.5
399.5
399.6
±
(Ma)
11.5
12.4
6.8
15.5
22.4
12.2
10.3
4.8
5.5
5.4
7.0
13.4
5.2
8.4
4.3
6.9
7.7
3.9
6.4
7.9
17.5
17.0
12.7
4.2
5.9
9.1
6.7
6.2
11.0
4.5
5.3
3.6
3.4
4.4
4.5
6.3
4.4
28.1
5.7
4.2
3.7
7.3
9.1
5.0
5.6
Conc
(%)
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
0.8, 0.8
FAR
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
400.0
400.1
400.2
401.1
401.3
401.4
401.4
401.7
401.8
402.5
402.6
402.8
402.8
402.9
403.0
403.1
403.5
403.6
404.0
404.3
404.6
404.7
404.8
405.1
405.4
405.6
405.6
405.8
405.8
406.0
406.0
406.0
406.2
406.2
406.3
406.5
406.7
407.2
407.3
408.2
408.5
409.3
409.5
410.0
410.8
410.9
412.4
412.6
412.7
413.6
413.6
414.5
2.8
5.6
3.3
3.2
3.4
2.0
5.9
14.4
5.8
3.7
4.6
3.6
8.0
2.5
5.1
6.0
4.6
5.5
14.4
3.3
15.5
7.1
10.1
4.9
8.4
5.4
5.2
5.5
5.0
3.5
8.4
4.0
3.4
4.2
9.2
2.0
2.6
5.7
4.1
8.1
13.7
7.0
2.6
3.5
3.0
3.7
4.7
5.2
3.6
12.7
6.1
7.5
NA
103.6
99.2
96.6
96.0
95.2
98.3
104.0
91.1
89.2
102.3
95.0
108.5
90.3
84.2
92.0
102.0
105.1
97.7
97.0
81.8
107.8
90.6
93.7
77.8
92.0
99.7
99.4
106.6
106.3
94.3
92.4
105.0
84.8
99.9
99.9
100.0
100.6
99.1
88.5
98.1
106.2
98.3
112.2
105.1
108.9
91.6
111.0
101.2
91.5
97.0
85.8
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
414.6
415.6
415.7
422.5
425.5
442.2
3.3
7.2
8.1
24.2
23.5
3.4
106.8
95.4
117.1
83.1
107.8
99.5
275.4
322.3
339.5
341.9
348.6
355.4
365.8
366.4
367.2
368.6
368.8
370.1
370.6
370.7
371.0
371.3
371.8
372.0
372.2
372.2
372.6
372.8
373.2
373.3
373.4
373.7
373.7
373.7
373.8
374.8
374.9
375.0
375.4
375.9
376.2
376.3
376.4
376.7
377.1
377.3
377.4
377.6
377.6
377.7
3.2
14.9
32.2
6.0
15.3
3.2
17.6
6.4
5.9
8.4
5.0
7.2
6.8
19.5
15.1
3.3
7.5
7.7
9.9
6.1
13.0
5.8
6.7
10.6
7.0
2.7
4.4
5.8
4.0
2.5
7.7
5.7
4.6
2.4
10.0
4.8
10.3
9.7
6.6
5.5
2.8
5.2
8.3
6.9
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
0.8, 0.8
FAR
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
377.7
377.7
377.8
377.9
378.0
378.0
378.3
378.3
378.6
378.9
379.0
379.1
379.2
379.2
379.3
379.6
379.7
380.2
380.2
380.3
380.5
380.7
381.0
381.0
381.1
381.2
381.4
381.4
381.8
382.0
382.0
382.1
382.6
382.7
382.9
383.1
383.7
384.0
384.0
384.2
384.4
384.5
384.7
385.0
385.6
385.8
386.0
386.4
386.5
387.4
388.5
389.1
3.5
3.5
5.4
7.6
9.3
5.2
12.8
8.6
9.9
2.6
7.3
4.6
7.0
10.2
4.6
6.7
4.9
4.1
7.9
4.8
3.3
6.1
11.1
3.6
4.0
4.9
14.2
10.7
5.1
6.6
6.3
9.2
4.8
7.0
4.3
3.3
4.1
4.0
3.7
11.1
2.3
5.3
12.0
5.6
5.3
15.9
4.0
5.8
9.5
4.8
4.2
17.7
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
389.9
390.1
392.1
7.2
16.1
9.6
NA *
NA *
NA *
288.4
302.9
315.1
325.0
326.2
328.2
331.6
334.4
344.6
347.3
350.2
352.8
353.3
353.4
353.9
356.4
356.7
357.1
357.4
359.6
360.7
362.1
362.1
363.2
364.9
365.4
365.5
365.8
366.0
366.1
366.3
366.5
366.8
367.3
367.4
367.6
367.9
367.9
368.1
368.3
368.4
368.5
368.8
368.9
369.0
369.3
369.5
3.8
13.2
8.9
16.3
20.3
13.1
10.1
13.7
9.1
3.3
5.2
7.7
10.5
4.5
6.0
3.4
18.0
21.8
7.5
4.1
5.4
6.6
10.9
3.6
2.3
10.9
3.3
3.2
8.8
5.5
3.8
4.2
22.6
5.6
4.7
2.6
2.4
2.8
3.9
5.4
7.1
13.0
7.3
4.7
2.9
9.0
3.3
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
0.8, 0.7
FAR
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
369.5
369.7
369.8
370.1
370.3
370.3
370.5
371.0
371.1
371.2
371.6
371.6
371.6
371.7
371.8
372.1
372.3
372.5
372.5
372.7
372.9
373.0
373.1
373.2
373.2
373.5
373.7
373.8
373.8
373.9
374.0
374.2
374.4
374.6
374.8
375.0
375.1
375.3
375.6
376.4
377.3
377.6
378.2
378.4
378.6
378.6
379.1
380.5
382.6
384.3
384.6
385.2
9.5
6.1
3.8
3.4
3.0
4.8
7.7
4.4
5.8
2.8
4.8
2.4
7.7
8.0
3.9
6.2
3.2
3.2
5.9
7.1
5.2
9.4
2.8
4.6
3.7
4.4
6.2
3.2
5.4
2.5
4.7
7.3
6.0
3.7
5.8
7.7
9.7
3.3
12.2
5.3
3.8
2.2
4.7
6.0
4.4
5.4
7.0
10.9
7.2
3.6
3.9
3.3
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
397.9
402.8
412.0
6.9
28.3
5.9
NA
84.3
107.3
93.0
94.3
270.3
367.4
373.9
408.1
417.5
422.9
428.0
428.3
431.6
435.6
435.8
437.5
442.0
442.1
442.7
444.0
444.2
446.4
446.6
453.8
458.3
480.9
481.1
484.2
1.7
1.0
12.7
17.7
17.4
3.8
14.8
6.4
5.7
10.3
4.6
10.0
19.5
4.8
11.3
6.9
16.2
2.7
7.3
6.2
8.2
3.3
12.6
11.7
29.5
19.6
NA
NA
NA
NA
NA
94.5
95.7
91.0
95.2
87.4
98.4
100.5
98.1
98.0
102.9
96.2
101.9
99.7
102.0
100.6
97.1
92.8
99.8
107.0
104.9
111.2
356.5
377.8
382.9
388.9
398.8
405.6
410.5
410.6
412.3
412.6
413.3
414.3
414.9
415.1
415.2
415.2
415.6
415.7
416.6
19.5
8.0
8.3
19.0
13.2
30.1
7.6
5.7
5.6
18.4
9.6
8.7
12.1
6.7
5.2
5.1
5.3
7.5
6.9
NA
NA
NA
NA
NA
NA
91.7
90.4
90.8
89.6
108.1
98.1
110.7
89.1
92.7
89.8
102.3
68.8
111.9
0.9, 0.8
IC
Metamorphic zircon
Metamorphic zircon
Metamorphic zircon
Metamorphic zircon
Discordant
Discordant
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
1.1, 0.8
FAR
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
*
*
*
*
*
*
*
*
*
*
*
*
*
416.8
418.0
418.0
418.7
419.0
419.1
419.2
419.3
419.4
419.7
420.0
420.4
420.9
421.3
421.5
421.9
421.9
422.0
422.1
422.3
422.3
422.7
422.8
422.9
423.0
423.0
423.0
423.2
423.5
423.5
423.9
423.9
424.4
424.6
424.9
424.9
425.1
425.3
425.8
425.9
425.9
426.0
426.1
426.5
426.5
426.5
426.6
426.8
426.9
426.9
426.9
427.0
7.0
5.1
6.1
7.0
5.2
4.1
10.5
5.7
9.9
3.4
7.6
6.4
6.3
7.5
5.6
5.3
12.8
3.2
17.4
5.4
5.8
6.0
7.8
7.5
6.6
8.4
6.0
8.5
3.6
6.4
6.9
14.3
12.1
6.5
9.0
8.1
5.4
6.0
14.6
4.8
4.7
8.3
5.7
4.3
8.9
7.0
18.3
2.9
4.2
8.7
8.5
4.7
105.7
100.7
96.6
95.1
97.3
97.1
95.3
93.3
93.2
90.4
101.1
85.5
100.3
83.8
94.7
95.9
98.8
99.5
109.5
96.4
86.0
88.1
98.7
93.8
95.7
109.8
102.5
103.4
96.7
98.4
89.3
100.4
107.6
103.5
122.8
93.4
96.2
95.6
100.7
99.4
97.3
97.9
89.4
102.3
96.8
94.2
95.9
96.1
99.3
109.9
97.7
89.6
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
428.5
428.5
429.0
429.2
429.3
429.4
429.5
429.7
429.8
429.8
429.9
430.0
430.9
431.2
431.3
433.3
433.5
434.2
434.6
440.4
441.4
444.8
451.6
13.4
13.0
9.2
6.6
9.2
9.0
5.7
5.4
5.0
3.8
8.2
5.9
12.6
23.7
9.1
8.4
3.3
15.4
8.1
10.8
22.1
40.1
11.1
95.7
100.3
101.6
98.4
98.0
95.6
96.8
98.6
106.7
98.1
89.3
104.3
99.8
97.6
101.7
90.8
103.0
106.4
94.6
110.3
75.9
101.0
94.5
384.3
391.3
391.4
394.1
395.2
396.3
396.9
397.0
398.0
398.2
398.3
398.8
400.1
400.1
401.0
401.4
401.9
403.1
403.1
403.2
403.9
404.1
405.3
406.1
414.2
418.9
422.1
7.9
7.8
8.5
9.3
3.9
9.6
6.2
11.1
5.0
7.2
23.2
11.3
7.7
11.1
5.9
15.4
8.6
14.9
4.8
7.5
13.7
6.6
5.1
5.4
7.7
12.5
6.2
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
94.1
105.7
103.9
96.4
96.4
102.9
95.9
92.6
105.6
101.2
92.8
106.9
98.9
85.4
105.4
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
*
0.9, 0.8
FAR
0.8, 0.8
FAR
NA Discordant
124.4
113.1
89.7
87.1
108.6
97.3
101.7
111.5
87.6
90.8
107.5
108.7
108.5
101.7
102.1
92.4
109.7
105.9
113.4
99.4
109.5
75.6
113.1
108.4
91.7
111.1
340.0
401.8
420.7
425.6
425.7
426.5
427.7
428.2
429.1
429.2
429.7
430.9
431.8
431.8
431.9
432.4
432.6
432.6
435.0
435.0
435.4
435.9
436.4
436.5
438.7
449.4
462.7
8.0
11.6
9.8
5.9
4.8
4.2
6.3
4.7
4.8
7.4
9.1
5.6
6.1
4.8
11.8
2.8
9.3
5.7
5.6
8.3
9.3
6.7
16.2
5.6
15.6
8.8
26.6
223.3
239.1
263.2
278.5
243.0
3.9
1.8
9.9
3.9
3.6
NA
NA
NA
NA
NA
96.8
137.7
157.2
237.0
240.7
242.7
244.6
251.5
251.6
251.7
252.1
253.0
254.3
257.5
0.9
9.1
4.7
5.1
4.4
3.9
1.5
3.9
9.9
2.8
6.7
2.6
12.7
6.0
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
0.8, 0.8
IC
Discordant
Discordant
Discordant
Discordant
Discordant
0.8, 0.8
FAR
258.3
258.6
258.8
259.1
259.1
259.4
259.5
259.7
261.4
261.5
261.6
261.6
264.7
265.0
265.4
265.7
266.8
266.8
266.9
268.6
283.3
289.8
292.9
299.2
351.0
357.8
413.9
433.4
1685.4
6.9
4.5
4.8
3.4
3.4
6.2
9.8
3.6
1.4
3.6
1.5
2.1
3.2
16.7
6.6
6.1
3.9
10.1
11.5
3.5
3.3
4.8
7.0
3.8
3.9
17.9
14.9
7.1
51.0
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
84.6
94.2
88.4
55.2
142.4
198.7
335.7
342.0
369.0
391.6
400.0
408.8
412.9
419.8
635.7
734.8
793.1
803.6
858.9
983.4
987.9
1027.8
1052.5
1071.9
1.0
4.1
2.0
1.7
6.2
2.4
13.1
3.1
13.4
6.5
7.8
7.2
17.1
13.7
33.6
11.3
40.9
16.9
14.7
29.9
16.6
NA
NA
NA
NA
NA
NA
NA
NA
93.6
94.0
81.6
99.0
94.7
80.1
85.1
91.3
89.9
89.5
92.5
84.7
94.3
1.0, 0.8
IC
Metamorphic zircon
Metamorphic zircon
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
1073.3
1078.9
1079.7
1082.5
1088.2
1094.3
1097.9
1099.2
1111.2
1139.7
1142.8
1156.9
1159.9
1181.3
1182.4
1193.3
1197.8
1259.0
1283.7
1323.5
1344.8
1362.1
1364.6
1386.3
1430.1
1437.1
1455.1
1473.1
1505.1
1547.7
1601.3
1611.2
1626.6
1629.0
1629.9
1633.8
1639.7
1653.2
1654.6
1665.7
1716.3
1726.2
1740.3
1743.0
1753.5
1851.3
1868.1
1883.8
1925.6
1967.0
2023.8
2076.2
19.0
12.1
16.2
32.0
24.4
33.5
16.3
13.5
16.3
20.1
22.8
12.3
31.5
10.0
11.5
15.5
25.4
18.5
17.4
15.0
15.6
12.0
20.7
89.8
25.1
16.3
17.8
12.9
15.4
67.9
16.4
16.0
15.1
16.1
12.8
21.2
11.3
21.0
17.4
11.6
37.2
14.2
26.7
10.0
18.2
15.0
10.7
10.9
19.2
15.9
12.2
18.4
92.5
96.8
90.5
80.9
81.0
98.0
96.7
85.7
89.7
86.7
100.5
98.6
84.4
95.8
91.8
89.2
82.9
84.3
95.3
99.6
91.7
90.6
92.3
81.7
89.9
91.4
93.6
85.4
90.8
90.3
85.7
83.8
95.4
99.8
89.6
86.6
81.4
84.3
90.2
88.7
93.4
93.1
86.4
95.4
97.7
92.7
80.3
88.3
85.3
91.2
94.1
94.8
2701.2
2705.9
2730.9
2825.9
2838.8
14.0
22.9
27.8
22.4
10.9
92.4
81.2
86.3
88.6
80.8
56.5
56.7
60.4
61.0
189.0
261.2
268.4
271.6
290.1
338.2
365.7
370.1
392.9
394.7
406.5
415.2
419.1
423.8
424.6
433.8
472.3
540.7
566.6
659.8
923.1
953.6
1013.5
1028.8
1029.9
1035.0
1075.5
1102.2
1126.1
1133.4
1139.7
1140.2
1145.5
1146.8
1162.9
1169.7
1228.0
1281.8
1301.1
1314.8
1325.3
0.8
0.5
1.5
1.9
5.9
22.7
9.9
15.9
14.0
4.8
6.7
12.1
23.3
8.2
24.4
6.8
3.9
19.5
14.0
11.4
20.5
34.9
11.1
59.1
24.3
39.5
62.9
20.4
14.5
123.8
35.3
4.3
61.3
21.7
34.5
40.8
39.5
111.6
64.9
8.6
19.0
31.8
117.7
6.9
23.3
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
93.2
92.3
94.2
99.3
97.7
115.2
139.2
49.8
101.4
96.0
97.7
99.4
95.3
93.2
96.0
99.7
99.3
89.6
93.2
93.2
96.5
98.5
95.7
98.0
91.2
95.0
84.8
84.1
87.0
89.5
87.1
0.9, 0.8
FAR
Metamorphic Zircon
Metamorphic Zircon
Metamorphic Zircon
Metamorphic Zircon
Metamorphic Zircon
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
1331.7
1374.8
1389.5
1419.0
1442.0
1451.5
1455.4
1457.1
1484.1
1484.3
1490.3
1493.8
1497.1
1498.5
1502.0
1503.4
1613.8
1615.0
1625.1
1646.8
1648.4
1648.9
1672.3
1706.0
1739.6
1744.5
1772.2
1792.1
1806.1
2003.8
2536.7
2668.2
2719.0
2966.9
43.5
16.7
16.6
71.2
6.7
16.3
8.7
7.5
26.9
12.1
15.6
14.8
4.1
31.2
13.3
3.0
16.6
5.7
17.7
28.0
5.1
10.0
7.7
7.9
13.1
15.3
6.9
8.1
4.6
10.0
12.9
12.4
2.7
5.9
67.7
72.2
78.1
81.7
83.5
83.6
83.9
84.2
88.8
89.8
92.6
93.4
95.4
96.5
97.7
102.1
1.4
0.7
2.5
1.2
1.5
3.5
2.2
1.9
6.6
3.6
1.1
3.4
1.1
0.9
1.9
4.3
97.5
96.4
40.5 Discordant
90.0
92.6
97.7
92.9
98.9
40.0 Discordant
92.8
90.3
95.6
92.7
90.8
91.0
98.4
91.3
80.9
99.6
83.9
92.1
84.0
92.2
81.8
92.9
96.9
93.8
98.1
93.4
80.6
84.0
98.6
86.1
94.8
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
metamorphic zircon high U/Th
103.7
109.6
119.9
119.9
160.2
178.8
180.7
190.7
199.0
200.4
202.3
206.2
206.7
210.2
210.8
3.4
3.3
7.6
2.4
11.3
12.2
1.9
2.9
3.7
4.8
8.7
7.7
2.5
2.1
5.9
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
Discordant
metamorphic zircon high U/Th
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
metamorphic zircon high U/Th
Discordant
metamorphic zircon high U/Th
Discordant
Discordant
83.3
86.2
87.0
88.5
88.9
89.2
89.7
90.8
91.2
91.4
94.1
94.5
94.9
95.3
95.9
102.7
110.6
141.3
160.7
161.6
172.9
176.2
176.2
178.6
182.2
196.5
342.6
2.9
0.8
2.6
2.3
1.9
0.9
2.0
2.4
1.1
1.7
0.9
2.8
2.4
0.5
3.6
3.2
5.5
3.2
7.5
2.5
1.7
3.2
2.5
2.0
5.0
10.9
5.8
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
Discordant
*
*
*
*
*
*
*
*
*
69.0
83.6
83.6
84.1
84.8
84.9
0.8
4.8
2.9
5.9
1.1
1.5
NA
NA
NA
NA
NA
NA
Discordant
1.0, 0.8
FAR
High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
84.9
85.4
85.4
85.4
85.5
85.7
85.9
85.9
86.2
86.2
86.2
86.3
86.3
86.4
86.6
86.6
86.7
86.7
87.2
87.2
87.2
87.2
87.4
87.5
87.5
87.8
87.8
87.9
88.1
88.2
88.5
88.7
88.8
89.0
89.2
89.2
89.4
89.5
89.6
89.6
89.6
90.0
90.2
90.3
90.6
91.0
91.2
96.3
97.0
1.3
2.1
1.1
1.4
0.9
2.6
2.3
1.4
0.6
1.6
1.6
1.0
1.1
1.4
2.3
0.9
1.5
5.0
1.1
0.4
1.1
0.8
1.6
1.1
0.5
4.2
5.4
1.4
1.0
1.5
0.8
7.1
0.8
2.1
2.2
0.8
1.4
0.5
4.3
4.5
1.4
4.9
1.8
0.7
4.1
5.2
0.8
3.8
1.7
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
* High U/Th and/or [U]…metamorphic zircon
High U/Th and/or [U]…metamorphic zircon
High U/Th and/or [U]…metamorphic zircon
High U/Th and/or [U]…metamorphic zircon
High U/Th and/or [U]…metamorphic zircon
High U/Th and/or [U]…metamorphic zircon
High U/Th and/or [U]…metamorphic zircon
High U/Th and/or [U]…metamorphic zircon
High U/Th and/or [U]…metamorphic zircon
0.7, 0.8
585.6
20.6
81.3
FAR
1246.1
1661.0
37.9
25.9
102.2
93.7
75.3
359.3
341.7
1.0
5.3
6.3
NA
NA
NA
260.1
326.9
362.6
371.9
374.6
375.0
375.8
379.6
383.4
383.5
383.9
387.3
391.4
395.8
10.4
12.3
6.7
6.6
11.5
4.6
4.2
4.6
7.5
8.7
11.4
7.0
16.4
16.0
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
57.2
60.1
78.8
79.9
81.4
82.1
82.5
83.7
85.0
87.8
90.4
92.6
101.7
104.3
115.0
234.4
249.5
264.2
280.7
299.1
309.5
331.7
347.3
354.3
356.9
357.3
357.3
1.9
1.3
0.6
2.6
2.0
1.4
1.2
7.5
3.3
0.9
0.6
2.2
9.8
3.0
2.6
5.4
15.0
11.9
15.7
4.2
6.9
4.2
5.2
2.6
2.1
7.0
10.9
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
0.8, 0.8
IC
0.8, 0.8
FAR
Discorant
*
*
*
*
*
*
*
*
*
*
*
*
1.2, 0.8
IC
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Disordant and high U/Th (Metamorphic zircon)
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
360.8
361.7
361.9
362.8
365.1
366.0
366.7
368.0
368.5
369.5
370.7
371.1
372.4
373.1
376.9
378.0
378.2
380.1
396.8
1.5
6.5
5.7
9.0
3.5
4.7
4.7
4.1
6.4
4.9
5.1
7.3
3.1
5.1
6.2
9.0
10.9
2.2
2.5
390.2
394.9
398.5
401.4
408.2
408.3
409.3
412.7
414.2
414.6
415.6
416.7
416.8
416.9
418.4
418.9
419.5
420.0
420.7
420.8
420.9
421.7
422.8
422.9
423.7
424.4
425.0
425.9
427.2
428.1
429.0
12.7
3.8
6.1
6.2
4.0
5.4
9.1
6.2
11.1
14.6
22.6
5.8
5.2
4.6
7.7
8.1
3.7
9.2
18.4
4.5
8.3
6.4
2.3
16.1
7.7
5.3
6.8
5.2
4.5
14.7
5.1
NA Discordant
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
*
NA
NA high [U]
1.0, 0.8
NA
NA
NA
85.1
83.9
96.4
98.4
98.2
101.7
106.1
114.9
104.9
101.7
101.2
126.4
99.8
88.8
119.7
112.9
101.5
99.6
96.8
98.2
119.8
95.6
92.1
108.4
101.0
104.0
111.5
137.1
FAR
429.3
429.5
429.6
429.7
432.6
432.8
433.1
434.1
434.2
434.4
436.0
436.3
437.0
437.1
438.6
438.7
438.9
439.3
440.8
441.8
444.3
445.1
445.9
447.0
448.0
448.3
449.8
449.8
452.7
458.6
465.5
468.1
468.9
469.9
471.5
491.6
495.6
497.2
504.2
508.3
508.4
511.1
515.2
531.3
552.5
611.1
650.0
908.2
963.0
1032.6
1045.3
1049.0
8.8
4.8
9.0
3.4
9.9
8.9
9.4
7.7
7.9
5.9
4.1
7.6
6.4
9.9
6.0
16.2
5.9
10.2
11.7
9.0
3.1
11.7
10.3
7.7
6.3
6.8
4.8
10.6
2.8
5.1
17.4
16.8
10.7
4.6
4.8
29.9
11.4
8.4
6.4
12.7
7.2
6.0
21.6
8.4
15.7
6.0
8.7
60.6
12.6
6.5
39.1
149.8
130.3
170.3
136.4
98.4
120.9
148.2
139.8
109.9
100.8
98.8
85.0
137.0
87.4
100.2
103.3
42.7
110.2
102.5
106.1
106.6
98.1
110.9
103.8
97.6
98.1
94.0
110.8
106.2
99.2
101.9
86.1
98.0
103.4
98.7
100.4
95.2
119.2
103.2
132.0
132.1
109.7
101.7
93.9
95.6
97.9
93.9
94.0
103.0
101.0
100.9
95.7
97.0
1069.9
1081.5
1083.7
1164.9
1207.7
1281.5
1494.9
1604.0
1608.8
1625.6
1637.3
1638.2
1665.4
1756.1
1815.8
1824.0
1830.3
1882.0
2196.3
2425.0
2675.6
2710.2
21.5
9.1
8.4
94.9
49.6
26.5
25.2
15.4
19.5
29.3
9.9
22.0
4.6
10.1
14.7
9.7
39.4
16.6
26.2
44.0
4.9
7.6
99.8
90.9
98.6
101.1
98.5
96.3
99.5
81.2
102.4
99.4
97.6
100.0
99.9
92.3
95.7
98.1
98.7
99.8
95.7
99.8
95.7
98.0
371.5
380.8
385.2
390.5
401.2
402.4
402.7
404.8
407.0
407.7
408.1
408.7
408.8
409.2
409.3
410.8
410.8
411.1
411.6
412.9
413.5
414.1
416.8
417.4
418.2
418.5
418.6
421.1
32.1
24.5
6.9
9.3
12.8
9.8
8.9
3.2
9.6
9.0
7.4
16.0
3.1
3.9
3.9
7.3
9.0
4.0
14.3
13.3
5.2
22.6
10.9
4.4
2.9
3.8
11.7
9.9
NA
NA
NA
NA
91.1
80.9
95.5
94.4
96.6
90.8
98.7
85.5
96.9
97.1
97.3
98.4
98.3
96.7
96.9
92.5
99.1
100.5
97.5
99.9
98.8
102.3
97.3
97.9
0.9, 0.8
FAR
422.3
422.7
423.0
424.0
424.5
424.6
427.4
427.8
427.8
428.3
428.5
428.7
428.9
430.3
432.1
432.5
432.6
433.0
433.1
433.4
434.2
435.3
435.5
438.2
440.9
441.8
442.9
447.3
449.7
451.2
452.5
452.7
455.8
455.9
456.7
456.7
456.8
458.5
459.6
461.6
464.8
468.3
469.0
470.7
472.6
473.4
487.3
491.2
493.2
505.8
550.6
555.9
14.3
7.0
21.2
6.8
3.9
11.0
6.5
6.9
2.7
5.3
3.0
9.6
9.1
14.4
7.2
3.3
2.8
5.4
5.7
4.7
4.2
8.3
3.0
5.6
8.0
3.9
5.5
9.4
6.5
6.0
3.1
6.3
8.2
6.0
5.1
7.7
8.1
7.8
7.2
10.7
12.6
6.0
8.7
7.6
5.8
6.5
4.8
3.3
8.6
7.9
9.9
16.0
101.9
78.7
102.7
96.8
99.5
141.5
94.5
93.9
101.6
96.8
99.9
118.7
92.4
76.5
101.1
93.4
110.0
110.0
100.6
93.4
98.0
95.0
95.4
104.8
96.5
97.7
101.1
96.1
86.2
95.4
97.6
98.9
104.2
91.5
94.0
101.0
111.1
103.4
102.7
123.1
116.4
103.6
101.8
99.6
102.4
98.4
101.5
100.1
88.2
91.8
96.1
100.9
560.8
564.9
565.8
565.9
566.1
568.2
568.9
586.3
599.0
607.9
647.6
662.3
663.1
687.0
936.1
955.4
981.6
1046.9
1075.6
1081.0
1121.9
1152.7
1159.2
1189.5
1368.3
1380.2
1453.1
1456.9
1618.7
1694.6
1761.2
1903.3
1998.3
2080.6
2558.7
2591.6
2595.7
2601.6
2867.1
2976.6
5.7
3.6
7.0
6.9
4.7
5.5
4.3
23.9
11.2
5.5
15.8
14.5
26.9
42.3
66.1
25.7
67.6
10.2
35.3
12.5
24.8
88.4
22.4
46.0
12.4
26.3
14.1
24.2
17.1
5.0
20.3
14.1
17.3
14.6
5.9
7.8
10.8
3.7
4.7
4.1
99.5
97.7
107.5
101.4
102.5
96.5
102.1
86.7
102.0
95.2
100.0
90.6
102.4
95.7
96.6
100.1
97.2
99.3
99.6
94.8
111.0
101.3
95.5
97.2
98.0
96.7
99.2
98.5
96.5
98.9
71.3
98.1
99.8
98.2
99.4
99.9
93.2
95.2
94.1
94.3
307.3
319.1
380.8
392.8
396.3
402.8
406.6
406.7
407.2
407.8
19.2
9.3
21.8
5.5
5.5
21.5
11.5
10.4
4.7
7.7
NA
NA
NA
NA
NA
87.0
92.6
75.0
95.6
95.9
0.8, 0.8
FAR
408.7
409.4
409.5
409.7
415.6
416.8
417.9
419.5
421.4
422.1
422.4
422.8
422.9
423.1
423.3
423.5
423.5
423.9
424.5
426.5
426.6
426.6
427.4
427.7
427.9
428.9
429.1
430.0
431.9
432.1
434.0
435.0
436.2
436.4
438.2
440.1
442.0
443.5
443.5
444.1
445.6
447.9
450.1
450.8
452.6
457.1
460.0
462.6
484.3
484.5
487.7
502.0
3.1
3.9
3.5
3.3
4.6
6.7
4.4
18.1
9.7
6.6
7.4
6.0
6.5
22.1
4.8
3.5
3.9
3.4
10.6
12.5
8.3
4.1
8.2
11.8
3.6
16.2
9.6
4.2
13.6
4.2
20.1
3.2
8.6
4.2
5.6
4.6
10.9
7.3
9.9
5.3
9.1
11.6
4.0
9.4
4.3
7.2
6.1
6.1
8.8
7.8
6.1
8.1
96.6
103.6
94.5
100.9
91.6
96.3
105.7
86.2
91.6
84.1
99.2
115.9
82.3
80.5
94.0
90.3
94.5
103.0
101.5
83.3
98.7
110.0
94.7
159.5
102.1
101.1
87.4
94.1
94.3
92.5
91.7
94.8
108.2
98.3
119.5
100.4
96.0
97.0
110.8
97.4
86.4
97.5
101.1
97.3
96.6
88.6
90.6
123.2
106.9
90.0
101.8
97.6
505.0
505.2
506.7
515.9
528.6
548.1
555.0
563.8
571.4
579.2
856.4
1032.2
1144.4
1153.8
1171.5
1176.8
1358.3
1458.3
1528.9
1692.8
1700.1
1719.7
1727.8
1873.3
1877.5
2173.0
2412.5
4.4
8.3
16.2
8.0
26.7
7.7
15.4
22.6
12.8
16.7
35.2
6.3
27.2
90.9
18.4
49.8
32.3
16.2
27.3
119.6
78.9
21.8
18.0
3.1
5.6
38.8
6.7
93.4
106.8
102.3
87.2
78.4
95.6
150.5
91.7
91.4
95.1
95.9
95.9
99.0
96.8
99.8
98.6
99.1
98.9
97.3
92.7
97.7
100.1
100.5
95.4
91.9
93.2
92.1
163.1
202.1
229.7
329.1
339.3
346.9
388.5
452.7
495.9
1078.2
1323.3
1429.0
1736.5
1742.2
1744.6
1752.4
1767.8
1768.2
1768.3
1770.3
1771.6
1774.2
1822.8
8.4
15.8
20.2
20.7
12.7
29.1
10.6
24.8
13.3
30.4
48.9
39.8
7.1
10.3
16.2
15.3
11.1
7.3
5.7
6.0
13.3
8.7
13.4
NA
NA
NA
NA
NA
NA
NA
37.5
42.8
98.8
38.4
32.3
82.4
88.4
93.0
84.8
91.1
82.0
86.2
91.0
97.4
94.1
86.2
0.8, 0.8
FAR
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
1825.6
1833.2
1838.7
1839.2
1852.9
1854.7
1856.1
1860.1
1875.1
1875.3
1918.5
1951.9
2067.0
2117.9
2142.7
2180.5
2422.9
2491.1
2521.6
2555.8
2605.6
2660.4
2670.2
2676.1
2676.9
5.6
25.7
12.6
8.4
13.2
19.5
16.4
7.9
6.6
15.1
12.6
13.2
9.3
9.2
6.8
26.8
7.5
5.3
5.6
5.6
12.5
5.1
6.0
9.8
54.9
84.5
93.5
103.4
91.6
91.5
97.4
97.3
89.5
90.2
82.4
85.4
91.2
88.6
94.3
92.9
21.5
92.9
86.7
90.8
90.3
93.8
80.8
95.2
87.0
93.1
313.6
322.9
328.3
336.0
337.4
338.8
340.2
343.6
343.9
344.2
345.0
345.1
345.1
345.2
345.4
345.8
346.1
346.1
346.2
346.4
346.5
346.6
346.6
346.9
346.9
8.6
16.3
7.5
31.1
3.3
16.5
6.0
14.9
5.9
6.6
4.9
10.4
3.3
6.7
5.4
3.4
5.0
2.9
4.7
3.3
3.1
5.0
7.1
10.5
3.5
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
0.9, 0.7
FAR
347.0
347.2
347.2
347.5
347.6
347.7
347.7
347.7
347.8
348.0
348.1
348.2
348.2
348.4
348.8
348.9
348.9
348.9
349.0
349.1
349.6
349.7
349.9
350.0
350.1
350.1
350.1
350.3
350.3
350.4
350.4
350.7
350.7
350.9
350.9
350.9
351.2
351.4
351.5
351.8
352.0
352.2
352.4
352.5
352.5
352.5
352.7
352.8
353.5
353.7
353.9
354.3
9.4
5.2
3.6
3.1
14.4
4.1
3.4
4.7
7.1
3.9
10.4
5.9
9.7
8.3
3.6
4.1
4.7
2.2
3.4
3.1
3.2
3.5
3.9
3.6
5.8
3.3
5.6
4.6
3.9
3.2
4.3
8.4
4.4
13.0
3.0
5.1
8.5
3.4
4.4
3.2
3.6
3.1
5.3
3.3
3.7
4.6
7.8
4.0
4.8
5.2
11.3
3.9
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
354.4
354.8
354.8
354.9
355.0
355.0
355.3
355.8
356.0
356.0
356.1
357.8
357.8
360.3
385.8
1336.7
1650.2
1772.4
1833.5
1927.4
2220.6
2744.8
19.8
6.0
8.4
3.6
3.2
11.5
12.5
3.3
17.2
5.1
4.1
7.9
2.8
5.8
32.5
5.4
8.3
4.5
26.7
11.1
22.6
6.9
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
97.2
100.7
87.1
99.6
100.0
89.3
100.7
342.6
344.1
344.8
345.2
345.8
346.2
347.3
347.5
347.9
348.3
348.8
348.9
349.3
349.3
350.2
350.6
350.8
352.0
352.0
352.6
353.4
353.9
354.3
354.3
355.4
356.3
356.7
357.4
5.9
2.6
2.8
8.0
12.3
4.3
5.0
5.1
4.8
4.7
3.9
3.0
2.5
3.5
15.2
8.6
8.1
3.6
3.4
2.6
7.5
6.5
14.8
3.8
3.5
5.7
4.5
5.1
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
1.1, 0.8
FAR
357.7
357.9
361.4
362.3
363.2
363.6
364.2
368.7
427.7
430.0
653.0
1087.4
1094.2
1149.8
1168.7
1248.8
1328.3
1354.4
1392.1
1631.7
1633.0
1644.6
1666.0
1739.1
1774.5
1774.9
1783.4
1785.3
1785.4
1793.9
1810.1
1824.6
1832.3
1835.6
1838.5
1840.8
1841.6
1844.6
1848.7
1854.1
1857.1
1860.5
1866.2
1875.1
1879.0
1891.2
1898.1
1915.0
1928.0
1931.8
1935.7
1988.7
7.2
6.6
4.5
3.0
11.6
3.6
9.9
10.2
10.6
6.9
7.7
33.3
23.8
39.0
72.8
99.4
13.1
10.5
32.5
14.3
8.8
22.5
30.7
34.1
19.7
13.0
8.2
8.3
9.7
2.7
13.0
13.4
14.1
26.9
15.7
5.9
4.3
25.6
22.9
23.5
9.3
21.1
22.7
12.0
46.6
47.6
70.2
11.5
10.1
6.9
39.9
8.1
NA
NA
NA
NA
NA
NA
NA
NA
122.5
125.1
94.8
98.0
97.2
99.9
100.2
102.7
100.2
95.3
99.5
99.5
96.9
95.5
97.1
100.7
101.1
99.2
98.4
100.7
99.2
94.6
96.8
99.3
101.4
100.5
102.4
102.1
101.0
99.7
98.4
98.3
96.8
98.4
102.6
98.0
97.2
101.2
100.6
99.8
99.3
98.6
99.2
100.9
1997.4
1999.4
2076.4
2165.3
2242.1
2323.9
2340.1
2380.3
2398.4
2484.4
2485.2
2599.1
2600.3
2609.2
2672.5
2694.0
2725.7
2766.2
2967.5
2968.0
2968.3
2968.3
2968.3
2968.8
3232.8
11.1
40.0
44.8
24.3
35.5
4.3
8.7
34.6
6.1
4.4
22.8
19.2
8.2
13.3
6.1
8.4
10.6
8.7
2.1
2.1
1.1
4.9
7.6
2.0
6.4
52.9
53.3
53.8
54.2
54.4
54.8
55.4
55.5
56.1
56.6
59.0
59.2
60.3
65.9
67.8
69.0
69.9
70.0
71.7
99.4
105.3
119.8
152.1
154.1
213.4
0.9
0.4
0.6
0.5
1.4
0.9
1.1
0.5
1.5
1.0
0.7
1.0
3.2
2.0
1.1
1.2
0.5
0.9
0.7
1.6
1.4
8.7
2.5
0.4
3.7
99.2
99.6
101.2
100.4
99.7
100.3
99.8
93.7
98.7
85.3
100.1
98.9
100.2
99.1
96.0
98.1
99.4
98.6
99.4
102.1
101.1
100.4
99.7
101.5
98.4
1.1, 0.8
IC
NA
FAR
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA Discordant
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
221.7
305.7
318.1
326.2
331.9
334.1
336.8
347.5
349.3
351.0
351.3
351.4
351.7
353.5
354.4
355.9
356.1
357.4
358.2
358.9
359.6
359.9
360.1
361.6
362.0
362.4
363.4
363.6
364.4
364.7
365.2
365.5
366.5
366.6
367.2
367.4
367.9
367.9
368.9
368.9
369.0
369.1
369.2
369.2
369.7
370.0
370.2
370.7
371.5
371.5
371.5
371.7
4.2
4.6
2.3
12.7
18.6
11.9
4.6
8.9
4.8
10.5
4.6
3.1
3.9
2.0
12.2
7.9
2.2
7.0
9.5
4.1
6.9
4.0
11.3
8.1
5.3
6.7
1.7
6.6
9.2
3.8
5.5
2.7
5.6
7.5
9.4
3.2
2.8
4.7
4.8
18.9
7.6
5.2
3.6
14.6
5.3
9.4
3.3
6.5
3.4
5.5
7.9
7.4
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
Discordant
371.9
371.9
372.0
372.3
372.4
372.5
372.5
372.6
373.3
373.9
374.0
374.0
374.3
374.5
374.6
375.2
375.8
376.3
376.6
377.7
377.9
378.8
378.9
378.9
379.4
380.5
380.5
380.7
380.7
381.3
381.4
381.4
381.4
381.4
381.5
381.8
382.3
382.3
382.4
382.6
382.9
383.5
383.9
384.9
385.4
385.4
385.7
386.4
386.8
387.5
387.8
389.9
2.3
7.3
4.8
15.6
5.3
11.5
3.8
3.5
4.0
8.9
6.5
5.9
9.8
6.5
4.2
3.5
6.6
4.2
4.0
3.8
4.2
2.2
2.0
5.8
5.7
8.1
4.0
4.0
6.3
3.9
4.0
3.6
5.6
6.6
2.8
1.4
3.5
7.9
7.0
5.0
5.7
5.8
8.1
6.4
7.1
6.5
7.4
5.2
6.3
5.8
5.2
6.0
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
390.4
397.6
398.5
405.3
405.5
1129.3
12.9
16.3
3.3
12.4
11.2
14.1
NA
NA
NA
88.2
115.0
100.4
60.0
60.8
61.2
61.3
62.4
63.9
98.2
1048.9
1181.4
1287.3
1345.3
1653.5
1679.8
1737.9
1795.4
1799.5
1807.6
1810.9
1816.5
1825.6
1827.6
1828.2
1829.0
1832.3
1832.5
1835.9
1836.6
1837.3
1839.6
1842.9
1843.6
1843.7
1843.8
1843.8
1845.0
1845.8
1846.0
1846.5
1847.2
1847.9
1848.0
1848.6
1851.6
1852.3
1.9
3.4
1.7
2.0
1.8
6.2
3.1
14.5
36.2
97.1
25.8
16.2
17.6
7.7
26.3
18.9
11.6
42.5
50.7
13.0
37.7
24.9
19.7
13.6
9.4
26.0
57.2
39.1
8.5
15.1
43.3
12.2
17.7
15.6
47.3
21.9
31.7
33.6
21.7
40.6
21.6
15.0
37.5
7.4
0.8, 0.8
FAR
NA
NA
NA
NA
NA
NA
NA
95.7
84.2
102.9
100.3
95.2
29.1 Discordant
94.4
100.8
100.3
98.8
82.5
96.5
96.4
99.6
100.1
99.0
97.4
90.3
96.2
88.1
97.0
95.6
95.9
100.3
97.6
97.7
99.3
97.9
99.9
98.3
99.8
99.8
99.2
95.8
94.1
96.5
98.4
1854.8
1855.2
1855.7
1855.8
1857.0
1858.5
1860.8
1861.1
1878.2
1887.5
1891.9
1893.8
1899.7
1900.2
1906.3
1907.5
1909.3
1911.3
1913.7
1916.7
1917.8
1918.6
1920.3
1926.2
1926.5
1928.7
1933.4
1936.5
1937.3
2055.7
2057.6
2070.3
2073.2
2080.3
2081.5
2325.7
2439.8
2543.5
2578.7
2609.5
2638.1
2690.8
2699.0
2710.0
2718.9
25.6
17.7
25.6
15.7
43.2
28.8
43.1
48.1
18.0
26.2
12.4
15.8
41.9
45.6
22.4
7.7
27.6
23.9
26.8
34.6
19.1
39.1
19.4
8.9
22.7
46.6
14.8
32.1
14.5
13.2
23.6
19.4
22.4
14.9
8.0
16.8
33.3
16.2
9.3
13.4
8.5
16.3
10.6
9.4
11.2
95.2
96.3
102.9
98.3
98.7
98.7
99.1
99.0
97.1
91.0
92.9
99.5
100.2
99.4
100.8
88.9
99.7
99.4
99.1
95.6
97.2
99.3
90.1
90.1
95.3
90.4
97.3
98.4
94.7
92.6
99.5
98.0
95.9
96.6
93.9
94.7
95.7
97.0
96.2
96.4
90.0
98.6
99.7
97.8
100.1
chemistry Geophysics Geosystems 9 (Q03017), 13
12MP09
20
15
DM
10
5
0
CHUR
-5
-10
-15
Epsilon Hf
-20
-25
-30
-35
-40
-45
-50
-55
-60
-65
-70
-75
-80
0
200
400
600
800
1000
1200
1400
1600
Age (Ma)
1800
200
DM Age
176Lu/177Hf
0.0036
0.0115
0.0193
00
2200
2400
2600
2800
3000
3200