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《Gansu Geology》 2018-Z1
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DISCOVERY OF DAQISHAN LEAD-ZINC POLYMETALLIC DEPOSIT IN SOUTHERN BEISHAN BELT

YE Hong-gang;FAN Xin-xiang;ZHAO Ji-chang;WANG Peng;XUE Bao-xian;The Fourth Institute of Geology and Minerals Exploration, Gansu Provincial Bureau of Geology and Minerals Exploration and Development;  
Daqishan lead-zinc(silver) deposit is the first continental volcanic hydrothermal Lead-zinc polymetallic deposit found in Gansu Province, located in the territory of Daqishan in the south of Beishan, Gansu Province. The output of the deposit is controlled by the Dongdaquan-Jinchanggou fault and the Hongliuyuan-Daqishan-Zhangfushan deep fault in the area, which is located at the confluence of regional faults and volcanic structures(volcanic structural depressions). The ore area is initially delineated 3 pieces of lead-zinc ore body,the orebody length is 1 196 m~2 500 m, the thickness is 1. 48 m~10. 01 m, the Pb + Zn is distributed between0. 536% ~12. 996%, the symbiotic silver, copper and tin, and silver is up to 800 × 10-6. Comprehensive mineralization geological background, geological characteristics, mineral distribution, ore-controlling factors and regional geochemical characteristics, We confirm that this area has the potential to form a large continental volcanic hydrothermal endogenous metallogenic deposit. Increasing comprehensive research and regional prospecting efforts is expected to obtain a breakthrough in prospecting. This prospecting discovery has important guidance and reference significance for finding Lead-zinc polymetallic ore and continental volcanic hydrothermal endogenous metal deposits in this area.
【CateGory Index】: P618.2
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