Tongshan Silver Ore Deposit Geological Characteristics and Ore-prospecting Criteria Analysis
Cheng Fen-we
Abstract
Cheng Fen-we
Abstract
xinjiang is located in the late Paleozoic silver,copper,gold polymetallic metallogenic belt,in east section of east Bogurda Tianshan-Halick,with favorable ore-forming geological conditions. Ore bodies are found in the marine-terrigenous sedimentary-volcanic clastic rock structure of Carboniferous Yamasu group,with significant tectonic ore-controlling characteristics. Combined with regional ore-forming geological background,analysis is carried out on the geological characteristics of the mining area,silver pb-zn orebody characteristics,ore characteristics and mineral paragenetic association characteristics. On this basis,the mining prospecting marks are summed up,pointed out the direction of looking for the same type deposits in the region.
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xinjiang is located in the late Paleozoic silver,copper,gold polymetallic metallogenic belt,in east section of east Bogurda Tianshan-Halick,with favorable ore-forming geological conditions. Ore bodies are found in the marine-terrigenous sedimentary-volcanic clastic rock structure of Carboniferous Yamasu group,with significant tectonic ore-controlling characteristics. Combined with regional ore-forming geological background,analysis is carried out on the geological characteristics of the mining area,silver pb-zn orebody characteristics,ore characteristics and mineral paragenetic association characteristics. On this basis,the mining prospecting marks are summed up,pointed out the direction of looking for the same type deposits in the region.
Key concepts: Prospecting, Geology, Geochemistry, Carboniferous, Paleozoic, Clastic rock, Terrigenous sediment, Sedimentary rock