Petrographic Report: Polished Thin Section SLD-05-03M Rock Type: albite-phyric lapilli tuff The thin section displays abundant lapilli of granular, interlocking quartz with two overprinting generations of alteration. The sample is weakly altered with almost 80% of the primary mineral assemblage remaining. The primary mineral assemblage was dominantly quartz lapilli, feldspar (albite > K-feldspar), quartz, albite phenocrysts, and K-feldspar spherulites. Lapilli make up about 40% of the thin section, range in size up to 3 mm wide, and commonly contain radiating fans of secondary biotite, epidote, and hematite, and rarely contain albite phenocrysts. The lapilli are locally rimmed by outward-radiating K-feldspar that is reminiscent of K-feldspar spherulites (Fig. 1). Rare K-feldspar spherulites up to 1.2 mm wide also occur within the section, typically with lapilli, and may contain inclusions of anhedral quartz and feldspar. Lath-shaped euhedral albite phenocrysts range in size up to 3 mm. The groundmass is felty-textured and composed of cryptocrystalline to fine-grained quartz and feldspar, likely with more albite than K-feldspar, although the grains are too small to accurately identify. This composition classifies the rock as an albite-phyric lapilli tuff. The hand sample is composed of rounded grey fused lapilli with white centres that are slightly flattened in one direction. Pink Kfeldspar spherulites are rare between lapilli. Small patches of rusty alteration occur throughout the hand sample. The offcut has been stained to check for the presence of K-feldspar, and it has taken on a slight pale yellow colour, indicating trace to minor amounts of K-feldspar. The two alteration events include an initial biotite- hematite-epidote alteration event followed by clay alteration of feldspar minerals, and lastly, an iron oxide alteration event. The first alteration event was a selective alteration of quartz lapilli by biotite, hematite, and epidote, accompanied by biotite veining in albite phenocrysts and groundmass, and hematite dissemination throughout the thin section. Biotite, hematite, and epidote overprint lapilli cores (Fig. 2) or rarely rims the cores, and rarely occur in clusters within the groundmass. Biotite in lapilli occurs as radiating fans and acicular aggregates that are rusty in places, and are rarely rhombic in shape. Hematite in lapilli occurs as bladed grains between biotite fans, while epidote occurs as subhedral prisms between biotite and overprinted by hematite. Within the groundmass, Mineral Modal Percent Abundance Primary rock Quartz 38 Feldspar 22 Albite phenocrysts 10 K-feldspar spherulites 3 Early biotite-clay-hematite-epidote alteration Biotite 12 Hematite 4 Epidote 1 Sericite Trace Clay alteration Illite-smectite 10 Iron oxide alteration Limonite Trace Lepidocrocite Trace Size Range (mm) Up to 0.4 mm Up to 0.1 mm Up to 3 mm Up to 1.2 mm Up to 0.15 microns Up to 1.2 mm Up to 0.2 mm Up to 0.1 mm Up to 10 microns Up to 30 microns Up to 0.5 mm biotite occurs as thin, wormy veinlets up to 0.03 mm wide and 1 mm long, which also rarely cut across albite phenocrysts. Hematite occurs as fine-grained disseminated anhedral grains and clusters up to 1 mm wide. More Cliffmont Sample SLD-05-03M Page 1 often than not, euhedral epidote is associated with hematite clusters. Hematite rarely fills fractures in albite, but does not occur as replacement of the phenocrysts. The mineral assemblage of the first alteration event is not typical of epithermal-style deposits. The second alteration event consists of very fine-grained felty-textured illite-smectite overprinting feldspar phenocrysts, in the groundmass, and spherulites. Illite-smectite also rarely occurs as patches within lapilli, where it may replace biotite. Replacement of albite phenocrysts and K-feldspar in spherulites by illitesmectite is weak, very fine-grained and generally replaces less than 5% of the crystal. The mineral assemblage of the second alteration event is indicative of argillic-style alteration. The last and final event for this rock was a late, weak iron oxide alteration event characterized by the overprinting of granular limonite on the groundmass and occasionally replacing biotite, accompanied by thin veinlets cutting the groundmass. The limonite veinlets are up to 0.02 mm wide and 2 mm long, and generally oriented SE. Trace lepidocrocite replaces hematite in places and occurs as needles or blades. Although weakly altered, the rock does not display much evidence of deformation. qtz K-fsp qtz py bt Figure 1: Photomicrograph of a lapilli composed of interlocking, granular quartz (qtz) and secondary fanshaped biotite (bt). K-feldspar (K-fsp) encircles the lapilli and radiates outward from it. Photo taken in cross polarized transmitted light. Cliffmont Sample SLD-05-03M ep bt hem Figure 2: Photomicrograph of hematite (hem) blades associated with fan-shaped biotite (bt) and euhedral epidote (ep) within a quartz (qtz) lapilli. Photo taken in cross polarized transmitted light. Page 2