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MINERAL CHEMISTRY AND SHRIMP U-Pb GEOCHRONOLOGY OF MESOPROTEROZOIC POLYCRASE-TITANITE VEINS IN THE SULLIVAN Pb-Zn-Ag DEPOSIT, BRITISH COLUMBIA

John F. Slack, J. N. Aleinikoff, Harvey E. Belkin, Christopher Mark Fanning, Paul W. Ransom

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Abstract

Small polycrase-titanite veins 0.1-2 mm thick cut the tourmalinite feeder zone in the deep footwall of the Sullivan Pb-Zn-Ag deposit, southeastern British Columbia. Unaltered, euhedral crystals of polycrase and titanite 50-100 μm in diameter are variably

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Small polycrase-titanite veins 0.1-2 mm thick cut the tourmalinite feeder zone in the deep footwall of the Sullivan Pb-Zn-Ag deposit, southeastern British Columbia. Unaltered, euhedral crystals of polycrase and titanite 50-100 μm in diameter are variably

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Available abstract

Small polycrase-titanite veins 0.1-2 mm thick cut the tourmalinite feeder zone in the deep footwall of the Sullivan Pb-Zn-Ag deposit, southeastern British Columbia. Unaltered, euhedral crystals of polycrase and titanite 50-100 μm in diameter are variably

Key concepts: Titanite, Geology, Geochronology, Allanite, Geochemistry, Epidote, Calcite, Mineralogy

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MINERAL CHEMISTRY AND SHRIMP U-Pb GEOCHRONOLOGY OF MESOPROTEROZOIC POLYCRASE-TITANITE VEINS IN THE SULLIVAN Pb-Zn-Ag DEPOSIT, BRITISH COLUMBIA — Research Paper | ScholarLens