1988Economic GeologyOpen access

Distribution, mineralogy, and geochemistry of gold and silver in the north end orebody, Rosebery, Tasmania

David L. Huston, Ross R. Large

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Abstract

Study of the spatial and mineralogical distribution of gold and silver in the Rosebery north end orebody indicates that both silver and gold are concentrated in massive sphalerite-galena-pyrite ore and barite mineralization. Six styles of gold mineralization have been recognized: 1) in massive sphalerite-galena-pyrite ore (the dominant occurrence); 2) in massive barite mineralization; 3) in the upper parts of pyrite-chalcopyrite pods; 4) in distal pyrite mineralization; 5) in footwall mineralization; and 6) in remobilized quartz-carbonate veins. Mineralogically, gold occurs as electrum. The grain size of electrum has a lognormal distribution, with most grains having dimensions of less than 25 μm. Silver occurs dominantly in tetrahedrite, and to a lesser extent, in galena. -from Authors

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Study of the spatial and mineralogical distribution of gold and silver in the Rosebery north end orebody indicates that both silver and gold are concentrated in massive sphalerite-galena-pyrite ore and barite mineralization. Six styles of gold mineralization have been recognized: 1) in massive sphalerite-galena-pyrite ore (the dominant occurrence); 2) in massive barite mineralization; 3) in the upper parts of pyrite-chalcopyrite pods; 4) in distal pyrite mineralization; 5) in footwall mineralization; and 6) in remobilized quartz-carbonate veins. Mineralogically, gold occurs as electrum. The grain size of electrum has a lognormal distribution, with most grains having dimensions of less than 25 μm. Silver occurs dominantly in tetrahedrite, and to a lesser extent, in galena. -from Authors

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Available abstract

Study of the spatial and mineralogical distribution of gold and silver in the Rosebery north end orebody indicates that both silver and gold are concentrated in massive sphalerite-galena-pyrite ore and barite mineralization. Six styles of gold mineralization have been recognized: 1) in massive sphalerite-galena-pyrite ore (the dominant occurrence); 2) in massive barite mineralization; 3) in the upper parts of pyrite-chalcopyrite pods; 4) in distal pyrite mineralization; 5) in footwall mineralization; and 6) in remobilized quartz-carbonate veins. Mineralogically, gold occurs as electrum. The grain size of electrum has a lognormal distribution, with most grains having dimensions of less than 25 μm. Silver occurs dominantly in tetrahedrite, and to a lesser extent, in galena. -from Authors

Key concepts: Sphalerite, Pyrite, Tetrahedrite, Galena, Geology, Geochemistry, Mineralization (soil science), Chalcopyrite

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Distribution, mineralogy, and geochemistry of gold and silver in the north end orebody, Rosebery, Tasmania — Research Paper | ScholarLens