Petrographic Report: Polished Thin Section SLD-13-02M Rock Type: carbonatized sub-arkose sandstone The thin section is a well sorted sandstone with less than 2% ovoid to rounded fragments. The hand sample is greenish-tan coloured and has parallel layering. In hand sample, the fragments are up to 6 mm long, ovoid to elongate, and burgundy-red in colour with thin green rims. Thin white veins cut the section in random orientations. Fine-grained pyrite is disseminated throughout the sample. In thin section, the primary mineral assemblage is composed of well sorted and fine-grained (up to 0.25 mm) detrital quartz, lesser K-feldspar, and minor albite, muscovite, and rutile. Quartz grains are subangular to subrounded, and minor pressure solution structures are occasionally present between grains. K-feldspar and albite grains are commonly blocky and subrounded, and rarely weakly altered to clay. Rutile grains are fine-grained, sub-rounded, and disseminated through the section. Detrital muscovite occurs in plates and laths. The few rounded fragments (less than 2% of the rock) are composed of medium-grained recrystallized carbonate and minor rounded, fine-grained quartz. These few fragments are composed of 80% carbonate, 10% quartz, and 10% pyrite. The original detrital composition classifies the original rock as a fine-grained sub-arkose sandstone (using the Folk 1965 sandstone classification scheme). The sample is overprinted by at least two generations of alteration. The two events consist of an initial, weak carbonate alteration with accompanying chlorite, pyrite, and epidote, and a later weak clay alteration dominated by illite-smectite and minor sericite. Alteration has not reduced grain size, and is largely confined to interstices between detrital minerals. The first alteration event was a pervasive but weak carbonate alteration of the host rock and recrystallization of fragments. Carbonate is fine-grained and largely found interstitially between detrital grains, but in some places overprints detrital muscovite. It also occurs in denser patches in places up to 1 mm wide. Fragments with coarser carbonate (up to 0.5 mm wide) are rimmed by anhedral, net-textured chlorite (rims up to 0.4 mm wide). Carbonate alteration was accompanied by pyrite crystallization. Pyrite is fine-grained, euhedral, cubic, and disseminated throughout the section. Pyrite occasionally bears inclusions of detrital rutile and quartz, and trace secondary chalcopyrite. Chalcopyrite also occurs as rare interstitial grains in carbonate. Mineral Primary rock Quartz K-feldspar Muscovite Albite Rutile Early carbonate alteration Carbonate Pyrite Chlorite Epidote Limonite Chalcopyrite Sphalerite Native gold? Late clay alteration Illite-smectite Sericite Cliffmont Modal Percent Abundance Size Range (mm) 57 6 1 1 2 Up to 0.25 mm Up to 0.1 mm Up to 0.1 mm Up to 0.05 mm Up to 0.15 mm 15 5 2 1 Trace Trace Trace Trace Up to 0.5 mm Up to 0.8 mm Up to 80 microns Up to 50 microns Up to 30 microns Up to 50 microns Up to 20 microns Up to 10 microns 9 1 Up to 80 microns Up to 25 microns Sample SLD-13-02M Page 1 Trace sphalerite also occurs as rare interstitial grains in carbonate. A single grain of native gold (Fig. 1) occurs associated with a pyrite grain in the groundmass. This alteration mineral assemblage is consistent with the propylitic alteration style. The second alteration event is very weak and comprised of very fine-grained, felty-textured illitesmectite and minor associated sericite overprinting carbonate. What appear as distinct white veins in hand sample are barely distinguishable from the rest of the sample in thin section (Fig. 2), and are identified as ribbons of material up to 0.5 mm wide with more abundant clay alteration than the surrounding rock. This alteration mineral assemblage is similar to the argillic alteration style. au rt clay vein py Figure 1: Photomicrograph of a grain of native gold (au) associated with secondary pyrite (py) formed during the carbonate alteration event. A grain of detrital rutile (rt) is also observed here. Photo taken in plane polarized reflected light. Cliffmont Sample SLD-13-02M Figure 2: Photomicrograph of the general finegrained, equigranular texture of angular to euhedral crystals and common mineral phases in this thin section. Photo taken in cross polarized transmitted light. Page 2