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《GEOLOGY OF ANHUI》 2000-01
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THE GEOLOGICAL FEATURES OF THE DAMIAOSHAN GOLD DEPOSIT, QUANJIAO, ANHVI

WU Li - bin, SUN Ya -li, CHENG Guang - wen, LI Xi - long (No. 312 Geological Party of Auhui Bureau of Geology and Mineral Resources, Bengbu 233040, China)  
The Damiaoshan gold deposit occurred in the middle member of the Sinian Dengying Formation. It is resulted from polymetallogenic reworking and sourced from post - magmatic hydrothermal solution and the detrital rock of the Dengying Formation. The Huangpo Fault is as the passage - way for its ore fluid and the sub - order NNE - trending fault zone acts as the main host.
【Fund】: “地理信息系统(GIS)应用于安徽东部地区金矿资源评价”部分成果
【CateGory Index】: P618.51
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