Geological characteristics and prospecting indicators of the Chaganchulu Ag-Pb-Zn polymetallic ore field,Dongwuqi,inner Mongolia
Luo Yuan-hong
Abstract
Luo Yuan-hong
Abstract
In the study of geological characteristics of the mining area,it is believed that the Chaganchulu Ag-Pb-Zn polymetallic deposit in Dongwuqi,inner Mongolia is late Yanshanian magmatic hydrothermal fluid and fracture-controlled sulfide polymetallic deposit.The late Paleozoic volcanic-sedimentary stratum is an important ore bearing country rock.And the close association of Yanshanian period potassium calcium-rich alkaline granite with metallic deposits in time and special distribution is an important prospecting indicator.
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In the study of geological characteristics of the mining area,it is believed that the Chaganchulu Ag-Pb-Zn polymetallic deposit in Dongwuqi,inner Mongolia is late Yanshanian magmatic hydrothermal fluid and fracture-controlled sulfide polymetallic deposit.The late Paleozoic volcanic-sedimentary stratum is an important ore bearing country rock.And the close association of Yanshanian period potassium calcium-rich alkaline granite with metallic deposits in time and special distribution is an important prospecting indicator.
Key concepts: Geology, Prospecting, Inner mongolia, Geochemistry, Stratum, Hydrothermal circulation, Sedimentary rock, Volcano