m
..
New Mexico Bureau o f Mines and MineralResources
Open File Report No. OF-327
U
U
U
BIOSTRATIGRAPHY AND PETROLEUM SOURCE-ROCKPOTENTIALl
PHILLIPS PETROLEUM CO. NO. 1 SUNLAND PARK UNIT WELL,
D O ~ Am~ COUNTY, NEW MEXICO
by B.W. iordine, E.B. Robertson,
and C.R. Yourig
Phillips Petroleum Company
Research and Services Division
Bartlesville, Oklahoma
February, 1986
U
U
U
'.
BIOSTRATIGRAPHY AND SOURCE ROCK POTENTIAL
#i SUNLAND
PARK UNIT
DONA ANA, CO., . N E W MEXICO
JOB
-.
No.
R h S REPORT
B.
E.
B.
w.
BORDINE,
-44
No. 2 8 0 5 A
"ICRQPALEQNTOLOGY
ROBERTSON, PALYNOLOGY AND SOURCE'ROCK
C.
R.
YOUNG, MANNOPLANKTON
PHILLIPS
PETROLEUM COMPANY .
RESEARCH AND S E R V I C E SD I V I S I O N
GEOLOGICALRESEARCH
AND S E R V I C E S BRANCH
BARTLESVILLE,
FEBRUARY,
OKLAHOMIL
1986
”
“I
Rock A n a l y s i s
BiostratigraphyandSource
of -the 81 Sunland Park Unit Well,
Dona Ana Co.,
New Mexico
EPS Report No.
*
2805A
,
INTRODUCTION
I n an attempt t oa g e - d a t e
the s e d i m e n t s p e n e t r a t e d
Sunland P a r k Unit well, Dona
Ana
f o r a m i n i f e r sa n dc o c c o l i t h o p h o r e s
by the #l
Co., New Mexico, p a l y n o l o g y ,
were u t i l i z e d .
The p l a n t micro-
are either t h o s e c o n s i s t i n g oflong-ranging
t a x a or t h e y are so b a d l y t h e r m a l l y a l t e r e d t h a t i d e n t i f i c a t i o n
not possible.
fossilsencountwed
”1
”j:
I
”1
I
“3
I
“1
I
4”
is
Microfaunalexamination of samples from this well y i e l d e d
Inoceramus prisms s u g g e s t i n g a Cretaceous age f o r the 18,090 t o
18,200.foot i n t e r v a l .
I n a d d i t i o n , the presence ofsmooth-valved
o s t r a c o d so c c u r r i n gt o g e t h e rw i t hn n l l u s c a na n de c h i n o d e r m
f r a g m e n t si n d i c a t e s
a marginalto
shallow-water d e p o s i t i o n a l
environment.
The Occurrenceofnannofossilsin
and18,220
f e e tp e r m i t s
this well between15,350
the age-dating of these d e p o s i t s .F i v e
d i s t i n c tz o n e s ,r a n g i n gi na g e
are recognized.
frommiddleEocene
t oC r e t a c e o u s
.,
4
I
S o u r c er o c ka n a l y s i sr e v e a l s
that there a r e three m a t u r i t y
’-
the s t u d i e di n t e r v a l .
A t h e r m a l l ym - t u r eu n i t ,
w i t h TAI valueshoveringaround
2+ is foundbetween11,050and
l e v e l sp r e s e n ti n
1 2 , 2 0 0f e e t .
The d e p o s i t s between 12,200and13-,000
f u i l y mature with TAI valuesrangingbetween
‘:I
4
f e e t are
3- and 4-.
These
l a t t e r sediments are predominantlygas-prone.Thosedeposits
foundbetween13,000and18,220
f e e t are t h e r m a l l y o v e r m a t u r e with
TAI valuesbetween
4- and 4, and with Ro ’ s r a n g i n g f r o n 3 . 5 4 t o
5.18.
No commercial g a s d e p o s i t s are known t o e x i s t with Ro
valuesabove3.2andtherefore
the l o w e ri n t e r v a l
of tYis well is
much too h o t f o r the p r e s e r v a t i o n o f s i g n i f i c a n t q u a n t i t i e s
of
gas.
SUMMARY
The rare p r e s e n c e of Inoceramus prisms s u g g e s t s a C r e t a c e o u s
The unitbetween
a g ef o r the 18,090 to 1 8 , 2 0 0f o o ti n t e r v a l .
15,750and18,090
f e e t was examined o n l y i n t h i n s e c t i o n a n d
it
was b a r r e n bf a n y a g e - d i a g n o s t i c f o s s i l s .
DISCUSSION
The m i c r o f a u n a l e v a l u a t i o n o f
the s u b j e c t well was based on
t h ee x a m i n a t i o n of washed r e s i d u e s from theinterval18,090-18,210
f t . ( 6 samples), androckthin.sectionsbetween15,850-18,210ft.
( 46 samples).
Washed ResidueExamination:
Threemajorfaunalelements
were n o t e di n the washed r e s i d u e :
the mst s i g n i f i c a n t b e i n g the Occurrence of Inoceramusprisms
between18,090-18,190
f t .A d d i t i o n a l l y ,e c h i n o i ds p i n e s ,
.L
.I
o s t r a c o d s ,a n da g g l u t i n a t e df o r a mf r a g m e n t sw e r e " o b s e r v e d .
ThinSectionExamination:
,
The mst prominentfaunalcomponentsnoted
i n the t h i n sect i o n s were e c h i n o d e r m f r a g m e n t s ( p r o b a b l y b r o k e n e c h i n o i d p l a t e s ) ,
Echinoidspines,and
m o l l u s c 'fragments.Inoceramus
prisms were
n o t e do n l yi n
the sample t a k e n a t 18,200 f t .
Rare, u n i d e n t i f i a b l e
fOramS are s p o r a d i c a l l y d i s t r i b u t e d t h r o u g h o u t
the i n t e r v a l .
’-
I;
I
Conclusion:
”
Based on the o c c u r r e n c e of rare Inoceramus p r i s n s , a
i
Cretaceousage
is^ s u g g e s t e d for the i n t e r v a l 18,090-18,200 f t .
The r e m a i n i n gi n t e r v a l
(15,750-18,090 f t . ) , t h a t was examinedfrom
t h i n s e c t i o no n l y ,
d i d n o tc o n t a i na g ed i a g n o s t i cf a u n a .
U“c
A marginal
to shallowmarinedepositionalenviroyment
i n d i c a t e d by smooth s u r f a c e d o s t r a c o d s , andsupported
molluscan-echinoderm.assemblage.
E. .W. Bordine
/-I
Approved:
E. A.
Stanley
,’
is
by the
Nannoplankton B i o s t r a t i g r a p h y
81 Sunland P a r k Unit Well
Dona Ana Co., New Mexico
EPS Report NO. 2805A
SUMMARY
Biostratigraphy:
.
Based on the examinationof
-_
ditch samples ( a p p r o x i m a t e l y
from the 15,350 f t . to 18,220 f t . i n t e r v a l o f
e v e r y 200 f t . )
the
well, the f o l l o w i n g ages a r e
P h i l l i p s #1 SunlandParkUnit
established:
Depth ( F t . )
-
M a r t i n i Zone ( N P )
16,650
17,360
Eocene
Middle
Early-Middle
Eocene
E a r l y Eocene
15,350'-15,560
15,620
16,680
Age
17,360
-
18,200
Late Pa.leocene
18,200
-
18,220
Cretaceous
Basedonnannoplanktondata,
p e n e t r a t e dm a r i n es e d i m e n t st h r o u g h
NP 16-17
NF' 13-15
NP 10-12
NP?
the #l Sunland P a r k U n i t well
,the i n t e r v a l 1 5 , 3 5 0 f t .
to
1 8 , 2 2 0f t .
I n c l u d e di n
this report are:
and Last species o c c u r r e n c e( F i g u r e s
range charts o r d e r e do nf i r s t
1 and21,
a chart
i l l u s t r a t i n g - t h eS t a n d a r dN a n n o p l a n k t o nZ o n a t i o n( M a r t i n i ,1 9 7 1 )
with their r e s p e c t i v e geologic ages, and a complete l i s t i n g of
nannoplankton t a x a (Appendix).
.
DISCUSSION
BIOSTRATIGRAPHY
Calcareous nannoplankton (planktonicmrine organisms) were
the 15,350 ft.-18,200 ft.
found in all samples examined through
interval from the #1 Sunland Park Unit well.. The preservation
of
the nannoliths ranges from excellent to poor, the
withmajority of
the specimens falling in the poor to fair range. This less than
optimal preservation ,results from calcite overgrowths, probably
caused by diagenesis. The nannoplankton zonation of 'this wellis,
of the
less preci'se than that which
.is ordinarily possible b3cause
podr preservation.
The sediments penetrated in'the specified interval were deposited under prevailing marine conditions. This conclusion is in
accord. with the presence of foraminifera recorded in thin-sections
from this interval.
Middle Eocene
-16-17
(15,350-15,560 ft.)
The association of Sphenolithus furcatulithoides,
- obtusus,
S.
S. radians, and Zygolithus bijugatus suggests
NP 16-17
an
age for
this interval.
-
Early to Middle Eocene
Np
13'15 (15,620-16,650 ft.)
This section is designated NP 13-15, &sed upon the following
assemblage: Discoaster kuepperi, Helicopontosphaera lophata, .
Nannotetrina cristatus, Sphenolithus furcatulithoides,S . obtu'sus,
S . radians, Toweis occulatus, and Tribrachiatus orthostylus.
-
-
Early Eocene. NP 10-12 (16,680-17,360 ft.)
This interval is defined by an association consisting of
Discoaster
diastypus,
lodoensis,
multiradiatus,
S. radians,
Fasciculithus tympaniformis, Sphenolithus primus,
'"-1
'
'
7
Tribrachiatus contortus, andT
. orthostylus.
Late Paleocene NP9-8 (17,360-18,200
ft.)
The following assemblage
.
. strongly indicates a late Paleocene
NP 9-8 age assignment:. Discoaster falcatus, D. mediosw, D.
-
-
4
megastypus, D
. multiradiatus, Fasciculithus involutus,F.
lillianae, F. tonii, F.
.
- tympaniformis, Heliolithus riedeli,HS . prispp., Rhombaster calcitrapa, Sphenolithus anarrhopus, and
mus
- -.
Cretaceous (probably mastrichtian) (18,200-18,220 ft.)
-
.
"
_
.
Although Cretaceous nannoliths are recorded uphole
(intermittently), they are interpreted as being reworked. The
sediments penetrated in the18,200 to 18,220 ft. interval,
however, areconsidered to be of Cretaceous age. Even though the
Cretaceous nannoliths encountered range .in age from toAlbian
Maastrichtian, the association of Arkhangelskiella cymbs-formis,
Ceratolithoides kamptneri, Lithraphidites quadratus, an5 Micula
spp. indicates a probablemastrichtian age for this section.
C. RYYou
Approved:
E. A. Stanley
References
Martini, E.,
1 9 7 1 :S t a n d a r dT e r t i a r ya n dQ u a t e ' r n a r yC a l c a r e o u s
Proc, 2nd Conf. P l a n k t o l i c
M i c r o f o s s i l s , 2; pp. 739-706.
NannoplanktonZonation.
I"
1
U<
-1
'3
. .
'
U
"
.
perch-Nielsen,
K.,
1979:
Cretaceousbetween
CalcareousNannofossilsfrom
the NorthSeaand
Aspekte der Kreide Europas.
the Mediterranean.
IUGS Series A, No. 6 , pp.
223-272.
U'
.-
1
-1
.
-'I
-7
-1
S i s s i n g h , W.,
Nannoplankton.
1 9 7 7 :B i o s t r a t i g r a p h yo fC r e t a c e o u sC a l c a r e o u s
Geol. Mijnbouw,
the
56, pp. 37-65.
"
.
.
. ..
. .
.,. .
.
.
.
I
.
.. . .
'
.. . .
. .
.
.
.... ... ... .
. , ..
i
I
I
:
:;.:. . ..
,
.. .. ..
. ,.,.
.
*:. .
.d'.
,
. . ,.. ..
..j .. :.. .; ... .
... .. . . . ..
. . .
. . . ..
..
. . ... . ..
.. . ... ... ...
. . .. .. .. ... .. . c
i
t.
. . .
:, :
...
. .. .. . .
.
APPENDIX E
S I SUNLAND PARK U N I T
DONA
ANA
CO., U.S.A.
N.M.,
.
C-R-YOUNG
PPGE
8/85
I
15350.-15360.
ARKHANGELSKIELLA CYMBIFORMIS( I),
BRAARUOOSPHAERA SPP.( I),
CERATOLITHOIDES ACULEUS( I),
CYCLAGELOSPHAERA REINHARDTII( I),
OISCOASTER CRUCIFORMPS( I)0
,
. SPP.( I),
KAMPTNERIUS MAGNIFICUS('
1). MICRANTHOLITHUS
SPP( 13,
NANNOCONUS SPP.( I)BUAORUM
,
GARTNERL( I),
Q. GOTHICUM( I),
RHABDOSPHAERASPP. ( 31,
R. VITREA( I),
SPHENOLITHUS ANAHROPUS( I),
S. EELEMNOS( I)S
,
. ELONGATUS( I),
S. FURCATULITHOIOES( I),
S. OBTUSUS( I),
S. SPP.( 4), TRIBRACHIATUS ORTHOSTYLUS( I),
ZYGOLITHUS BIJUGATUS( 31,
15330.-15400.
,
I)SPHENOLITHUS
,
SPP.(
RHABDOSPHAERA
SPP.(
I),
. . 15430.-15440.
BRAARUOOSPHAERA BIGELOWII( I)GONGYLIS
,
SPP.( I),
MICULA SPP. ( I),
PLAGIOCLASE (TWINNED FELD ( I),
QUADRUM TRIFIDUM( 11, RHABOOSPHAERAMORIONUM(
I),
SPHENOLITHUS INTERCALARIS( I),
S. OETUSUS( I),
S. SPP. ( I),
TRIQUETRORHABDULUS SPP. ( I),
ZYGRHABLITHUS SIMPLEX( I).
.)
15530.-15560.
OISCOASTER OEFLANOREIC I)D.
, SPP.( I),
NANNOCONUS SPP.( I),
RHAEDOSPHAERA MORIONUH( I)R.
, SEMIFORMIS( I),
SPHENOLITHUS MORIFORMIS( I),
S. OETUSUS( I),
S. RADIANS( l ) , * S - SPP.( I),
TRIERACHIATUS ORTHOSTYLUS( 21,
TRIQUETRORHABDULUS SPP.( I),
15620.-15650.
CALCISPHAERULIDAE( I),
CERATOLITHOIOES ACULEUS( I ) ,
CONUSPHAERA MEXICANA( I)HELICOPONTOSPHAERA
,
LOPHATA( I ) ,
MARTHASTERITESFURCATUS(
I),
PLAGIOCLASE (TWINNED FELD.)( 13,
BUAORUM GARTNERI( I),
RHAEOOSPHAERA INFLATA( I),
R MORIONUM( l)R,RUDIS( I)SPHENOLITHUS
,
OBTUSUS( 2 ) ,
S. ORPHANKNOLLI( 21, S. PSEUOORAOIANS( I),
s. SPP.( 21, TRIBRACHIATUS
ORTHOSTYLUS( 41,
.
15710.-
'40
-
CERATOLITHOIOES ACULEUS( I),
DISCOASTER DEFLANOREI( I),
D. KUEPPERI( I)FASCICULITHUS
,
SPP. ( I),
GONGYLIS SPP. ( I),
MICRANTHOLITHUS.SPP( I), NANNOTETRINA CRISTATUS( I),
RHOMBDTER CUSPIS( I),
SPHENOLITHUS CONSPICUUS( I),
S. RADIANS( I),
S. SPP.( I),
TOUESISEMINENS(
I),
TRIBRACHIATUS ORTHOSTYLUS( I),
ZYGOLITHUSBIJUGATUS(
I),
c
APPENOIX B
*I
SUNLAND
PARK
UNIT
C-R-YOUNG
DONA
ANA
CO.,
N.M
-,U.S.A.
PAGE
2
8/8i
15920.-15950.
BRAARUOOSPHAERA BIGELOWII( I),
FASCICULITHUS SPP.( I),
LITHOSTROMATION PERDURUM( I),
PLAGIOCLASE (TWINNED FELD.)(
QUINQUERHABOUS COLOSSICUS( I),
SPHENOLITHUS
FU~CATULITHOIDES(
11, s. SPP.( I),
TRIBRACHIATUS ORTHOSTYLUS( I),
"1
I),
16220.-16250.
CALCISPHAERULIOAE( I)CERATOLITHOIDES
,
ACULEUS( I),
C. ARCUATUS( I),
HELICOPONTOSPHAERA SPP( I),
MARTHASTERITES SIMPLEX( I)BUAORUM
,
GOTHICUM( I),
RHABDOSPHAERA
SPP.(
I)RHOMBASTER
,
CUSPIS( I),
SPHENOLITHUS OBTUSUS( I),
S. ORPHANKNOLLI( 13,
S. RADIANS( 21, TRIBRACHIATUS ORTHOSTYLUS( I),
ZYGOLITHUS BIJUGATUS( I),
//
/'
16490.-16520.
BRAMLETTEIUS V A R I A B I L I S ( I),
SPHENOLITHUS MORIFORMIS( I),
S. SPP.( I)ZYGOLITHUS
,
BIJUGATUS(
I),
16620.-16650.
.
HELIOLITHUS SP.(
I)ZYGOLITHUS'BIJUGATUS(
,
I),
16680--16700..
ERAARUDOSPHAERA BIGELOWII( I),
CALCISPHAERULIOAE( I),
CERATOLITHOIOES ARCUATUS( 21, C. KAMPTNERI(, I),
DISCOASTER OIASTYPUS( 21, D. LODOENSIS( I),
FASCICULITHUS
HAYI(
I], F. SPP. ( I), MICRANTHOLITHUS
SPP ( I),
BUADRUM GOTHICUM( I)8,
. TRIFIOUM( I),
RHABDOSPHAERA SPP. ( I),
SPHENOLITHUS FURCATULITHOIOES( I),
S. ORPHANKNOLLI( I),
S. RADIANS( 21, S. SPP-( 13,
TRIBRACHIATUS ORTHOSTYLUS( 21,
TRIQUETRORHABOULUS INVERSUS( I),
16820.-16850.
CERATOLITHOIOES
KAMPTNERI
( 21, EIFFELLITHUS SPP ( I],
BUADRUM GOT,HICUM( 21, RHABDOSPHAERA INFLATA( 21,
R. MORIONUM( 21, R.-VITREA( I),
SPHENOLITHUS SPP.( 21, '
TRIBRACHIATUS ORTHOSTYLUS( 31, ZYGOLITHUSBIJUGATUS(
I),
171so.-171ao.
ARKHANGELSKIELLA
CYMBIFORMIS(
13, CERAT~LITHOIOES
ACULEUS( 11,
CHIASMOLITHUS
SPECIES(
11, OISCOASTER
CRUCIFORMIS
( I),
D. DIASTYPUS( 21, 0 . MULTIRAOIATUS( 1).
PLAGIdCLASE (TWINNED FELD.) ( I)
QUADRUM
,
GOTHICUM ( I),
RHABDOSPHAERA INFLATA( 21, R. MORIONUM( I),
R. SEMIFORMIS( 21, SPHENOLITHUS ANAHROPUS( I),
S. CONSPICUUS( I);
S. OELPHIX( I)S,
. PRIMUS( 21,
*I
"1
APPENDIX
01 SUNLAND PARK UNIT
C .R .YOUNG
".-
1
,
B
DONA
ANA
CD.,
N.M.,
U.S.A.
PAGE
3
8/8i
s.
RADIANS(
I), s. SPP.( I), TRIBRACHIATUS
CONTORTUS( I),
T. ORTHOSTYLUS( 31, TRIQUETRORHABDULUS INVERSUS( Z),
ZYGOLITHUS BIJUGATUS( 6),
17330.-17360.
I),
DISCOASTER DIASTYPUS( I),
BIANTHOLITHUSSPARSUSi
FASCICULITHUSTYMPANIFORMIS(
3), LITHOSTROMATION OPEROS'JM( I),
RHABDOSPHAERAMORIONUM(
I)SPHENOLITHUS
,
ANAHROPUSC I),
S. PRIMUS( I),
S. SPP.( I), TRIBRACHIATUS ORTHOSTYLUS( 31,
17360.-17330.
BRAARUOOSPHAERA
SPP.(
1). CERATOLITHOIDES ACULEUS( I),
DISCOASTER DEFLANDREI( I),
FALCATUS(
0.
I), .
D. KUEPPERI( I),
D. MEGASTYPUS( I)FASCICULITHUS
,
SPP. ( 2 ) ,
F. TYMPANIFORMIS( Z), NANNOCONUS
SPP.(
I),'
RHABDOSPHAERA
SPP.(
Z), RHOMBASTER CALCITRAPA( 3),
SPHENOLITHUS ANAHROPUS( 3); S. SPP. ( I),
TRIBRACHIATUS ORTHOSTYLUS( 4), ZYGOLITHUS.BIJUGATUS( I),
i
"1
"1
""1
""1
._
17450.-17480.
I)DISCOASTER
,
MULTIRADIATUS( I),
CERATOLITHOIDESKAMPTNERI(
PLAGIOCLASE (TWINNED FELD.) ( I)RHABDOSPHAERA
,
SPP. ( 4),
R. VITREA( I)SPHENOLITHUS
,
CONSPICUUS(
I),
S. RADIANS( I),
TRIBRACHIATUS ORTHOSTYLUS( I),
TRIQUETRORHABDULUS SPP.'( 21, ZYGOLITHUS BIJUGATUS( Z),
17600.-17630.
CERATOLITHDIDES
,
ARCUATUS( I),
CALCISPHAERULIDAE( I)
DISCOASTERMEGASTYPUS(
I),
FASCICULITHUSLILLIANAE(
I),
F. T O N I I ( I),
SPHENOLITHUS ANAHROPUS( I),
17330.-17960.
I)DISCOASTER
,
DEFLANDREI(.l),
COCCOLITHUSGAMMATION(
F. TYMPANIFORMIS( Z),
FASCICULITHUS SPP.( I),
LITHRAPHIDITES ACUTUM( I),
SPHENOLITHUS ANAHROPUS( Z),
S. CONSPICUUS( I),
S. SPP.( I)TRIBRACHIATUS
,
ORTHOSTYLUS( I),
TRIQUETRORHABDULUS SPP.( 1). ZYGOLITHUSBIJUGATUS(
I),
17360.-17990.
"11
I,
ARKHANGELSKIELLA CYHBIFDRMIS(
3),
BRAARUDOSPHAERA BG
I ELOW(I
I),
BRAAURDOSPHAERA
SPP.
PLATLETS( I),
CALCISPHAERULIDAE( 6),
CERATOLITHOIDES ACULEUS( 2), C. KAMPTNERI( 2),
COCCOLITHUS MIOPELAGICUS( I),
DISCOASTERFALCATUS(
I),
D. MEGASTYPUS( I),
FASCICULITHUS SPP.( 31,
F. TYt@ANIFORMIS( 4), HELIOLITHUS SP.( 21,
MARTHASTERITESFURCATUS(
1);MICULASPP.(
I),
PLAGIOCLASE (TWINNED FELD.) [ I
), QUADRUM GOTHICUM( I),
RHABDOSPHAERA SPP.( Z), SPHENOLITHUS ANAHROPUS( I),
1
"
'
1
APPENDIX B
"
".
,.
01 SUNLAND PARK UNIT
1
C-R-YOUNG
DONA
ANA
CO., U.S.A.
N.M.,
.PAGE
8/85
4
"
S. CONSPICUUS( I),
S: SPP.(
I),
THORACOSPHAERA SPECIES( 31,
TRIBRACHIATUS ORTHOSTYLUS( 51, ZYGOLITHUS BIJUGATUS( 21,
17980.-18020.
CALCISPHAERULIDAE('2);CERATOLITHOIOES
ACULEUS( 13,
c. KAMPTNERIC 13, .SPHENOLITHUS ANAHROPUS( 31,
THORACOSPHAERA SPECIES( I),
TRIERACHIATUS ORTHOSTYLUS( I),
ZYGOLITHUSBIJUGATUS(
I),
18050.-18080.
ARKHANGELSKIELLA CYMEIFORHIS( 2). EIFFELLITHUS SPP.( I),
FASCICULITHUSTYMPANIFORMIS(
21, MARTHASTERIXES FURCATUS( I),
-
..-
u
v.
3'
:'I
I
u',
-.
.
'
18170.-18200.
BONETOCARDIELLA CF. CONOIDEA( I),
CALCISPHAERULIDAE( l),
CERATOLITH~IDES
KAMPTNERI
( 21, DISCOASTER DEFLANDREI
( I),
0- FALCATUS( I),
0. KUEPPERI( I),
0. MEDIOSUS( I],
0. MULTIRADIATUS( 21, FASCICULITHUSINVOLUTUS(
I),
F - L I L L I A N A E ( I),
F. MAGNUS( 11, F.
SPP.(
41,
F. TYMPANIFORMIS( 2). HELIOLITHUSRIEDELI(.I),
H. SP.( 31, RHABDOSPHAERA SPP.( 2). SCAMPENELLA SPECIES( I),
SPHENOLITHUS ORPHANKNOLLI( I)
S.
, SPP.( 31,
THORACOSPHAERA SPECIES( 31, TRIERACHIATUS ORTHOSTYLUS( I),
ZYGOLITHUSBIJUGATUS(
41,
]
6 -.-
"7
T
u j.
18200.~18210.
ARKHANGELSKIELLA CYMBIFORMIS( 21, CALCISPHAERULIDAE( I),
INVOLUTUS( I),
FASCICULITHUS
,
DISCOASTER SPP.( I)
F. MAGNUS( I),
F- SPP.( I)NANNOCONUS
,
SPP.( 2),
PLAGIOCLASE(TUINNEDFELD.)(
21, RHABDOSPHAERASPP.(
I),
RHOMBASTER B I T R I F I D A ( I)THORACOSPHAERA
,
OPERCULATA( 21,
T. SPECIES( 5 ) , TRIBRACHIATUS ORTHOSTYLUS( I),
T
.
MICRANTHOLITHUS SPP( I)PHANULITHUS
,
OVALIS[-1);
BUADRUM GARTNERI( 1). SPHENOLITHUS ANAHROPUS( I),
S. OETUSUS( I)S,
. PRIMUS( 11, S. SPP.( I),
THORACOSPHAERA OPERCULATA( 11, T. SPECIES( I),
ZYGOLITHUS BIJUGATUS( 21,
1
?I
18210"18220.
'
ARKHANGELSKIELLA CYMEIFORMIS( I),
CALCICALATINAALTA(
I),
CERATOLITHOIDESHANAI(
I)C.
, KAMPTNERI( 2).
CYCLAGELOSPHAERA REINHAROTII( I)EIFFELLITHUS
,
SPP.( 21,
LITHASTRINUS GRILLII( 21, LITHRAPHIDITES ACUTUM( 2).
MICULA SPP.( I)NANNOCONUS
,
SPP.(
41, PHANULITHUSADDITUS(
I),
P. OVALIS( I)
PREDISCOSPHAERA
,
CRETACEA( I),
QlJADRlfM NITIDUM( I)RUCINOLITHUS
,
H A Y I I ( I),
THORACOSPHAERA SPECIES( 41, TRIBRACHIATUS ORTHOSTYLUS( I),
TRIQUETRORHABDULUS SPP.( I),
ZYGOLITHUS DIPLOGRAMUS( I),
-1-1
'7
-..
.
Y
APPENDIX B
01 SUNLAND PARK UNIT
DONA A N A CO.,
N.M-;U.S.A.
C-R-YOUNG
PAGE
8/36
18210.-18220.
ARKHANGELSKIELLA CYMBIFORMIS( 23,
BRAARUDOSPHAERA AFRICANA( 11, CALCISPHAERULIDAE( 21,
CERATOLITHOIDES ACULEUS( 11, C. ARCUATUS( 11,
LITHASTRINUS GRZLLIII 1); LITHRAPHIDITES ACUTUM( I),
L. WADRATUS( I),
MARTHASTERITES FURCATUS( I),
H. SIMPLEX( 11, NANNOCONUS SPP.( 11,
PLAGIOCLASE (TUINNED FELD.)(
11, QUADRUM GARTNERIC I),
THORACOSPHAERA SPECIES( 31, TRIERACHIATUS ORTHOSTYLUS( 11,
ZYGOLITHUS BIJUGATUS( 21,
. -.
-3
u.
w:
a
LEGEND:
(VA)
VERY ABUNDANT
(A) = ABUNDANT
(C) = COMMON
(R) = RARE
(VR) = VERY RARE
(RH) = REUORKED
( 1 ) = QUESTIONABLE
(CV) = CAVINGS
(CF) = CLOSE AFFINITY
.
Y
5
K1
LHHK I
09/23/85
'
I
CORE
SUNLAND PARK UNIT #'I, DONA ANA COUNTY, NEW MEXlCU
SOURCE ROCK GEOCHEMICAL AND VISUAL KEROGEN DATA
ZZZZZiZ CUTTINGS
I
s1 PEAK
52 PEAK
to
15
"-
mg per gram
3 per gram of r o c k
3
VITRINITE REFLECTANCE
HYDROGEN INDEX
PRODUCTION INDEX
0.s
L
VISUAL KEROGEN TYPfNG
T AI
normullzed percent
percent
I
*
THERMAL ALTERATION INDEX
1
1.5
9
c
I
I + 2d 2
1). 3-
.-
c
0
3 3+ 4- 4
so
I
I
.
.
.
,
100
-
I
"
4
0
2
1
4
I?
P
i
3.54
3.89
0
1
3.8%
c
I
9
2
1
3.92
3.77
3.60
0
3.SG
3.63
3.50
1.89
;;i;
3.43
3.4%
3.97:
3.x3.91
4.69
4.84
5.11
5.13
5.16
4.96
4.7 s
4
m-
4.6&
4.9 e-
c
S,UI
91
-
l
,
.
r
l
1
..,. .,..
2
w t % of rock
q
3
0.0
0.5
1.0
1.J
rng per gram of rock
0
0
,,,,
I
5
, . , ,
I
10
."',"'
1s
r : g per gram of r o c k
-
,
0.0
C.l
0.2
0.3
SI/(SI+S2)
d.4
9
"
%
s
1
o
-
4
u
l
4
a.
c-
20
40
. eo
(s1 x 1QO) /
sa
TOC
I
0
I
200
.
"
l
(52 X 100)
.
'
40 o
.
/ TOC
t
percent
IYYATVR~
1
I + 2-
.
2
MATURE
zt 3-
3
: O R Y 0.4
J + 4-
4
T AI
ALG
EX1
1
Ez%izz5
t
t
K
LIQUID P R O N E
"
1
GAS FRONE
K