Webveins, with a gangue assemblage of quartz + sericite + calcite + kaolinitc(?) + epidote + chlorite, and a variety of base and precious metal minerals. The coexistence of vapor- and liquid-rich fluid inclusions in vein quartz shows that the molybdenite-bearing anhydrite and quartz veins formed at 360 ø to 410øC from boiling, low-salinity brines. WebApr 1, 2024 · The quartz segregations occur at the margins and within the aplite dykes. a & b are from within the Yerington Mine (Yerington porphyry deposit). c is drill core from the Ann Mason porphyry deposit. These textures are likely akin to previous descriptions of ‘parting veins’ in porphyry systems elsewhere (Kirkham and Sinclair, 1988).
Descriptive model of Porphyry Sn - USGS
WebJun 2, 2024 · This fluid is forced to the edge of the granite pluton and forms thick veins or pods. The fluid apparently solidifies rapidly at relatively high temperatures, under conditions that favor a few very large crystals rather … WebJun 1, 2024 · The seven porphyry deposits observed today at Cobre Panama were likely produced by normal faulting that dismembered and tilted two or more originally upright … tempe from phoenix
Quartz solubility in the H2O-NaCl system: A framework for …
WebThe B veins are composed mainly of quartz, chalcopyrite, and pyrite, formed within the chlorite-sericite alteration zone, and remnants of magnetite are still found. ... ... The 5-10 … WebIn general, porphyry deposits are characterized by low grades of ore mineralization, a porphyritic intrusive complex that is surrounded by a vein stockwork and hydrothermal … Webin the valley bottom, with outcrops of porphyry vein stockwork plus sericite alteration. Drilling discovered the Kupfertal porphyry Cu-Au deposit (biotite ~10.7 Ma) at depths of 200-400 m below the valley floor, with grades up to 0.4 wt% Cu and 0.4 g/t Au, largely below the valley that bisects this world-class high-sulfidation district tempe fry\u0027s electronics