Latitude: 32°9'30"N
Longitude: 118°58'0"E
栖霞山铅锌锰银矿
Stratabound deposit, initially a SEDEX-type deposit hosted in Carboniferous dolomite, limestone, shale and sandstone, which was later overprinted by a skarn system associated with Yanshanian magmatism.
References
- Yuanming Pan and Ping Dong (1999): The Lower Changjiang (Yangzi/Yangtze) River metallogenic belt, east central China: intrusion- and wall rock-hosted Cu-Fe-Au, Mo, Zn, Pb, Ag deposits. Ore Geology Reviews 15, 177-242.
- Lianxing Gu, Khin Zaw, Wenxuan Hu, Kaijun Zhang, Pei Ni, Jinxiang He, Yaotong Xu, Jianjun Lu, and Chunming Lin (2007): Distinctive features of Late Palaeozoic massive sulphide deposits in South China. Ore Geology Reviews 31, 107-138.
- Yanjing Chen, Huayong Chen, Khin Zaw, Pirajno, F., and Zengjie Zhang (2007): Geodynamic settings and tectonic model of skarn gold deposits in China: An overview. Ore Geology Reviews 31, 139-169.
- Khin Zaw, Peters, S.G., Cromie, P., Burrett, C., and Zengqian Hou (2007): Nature, diversity of deposit types and metallogenic relations of South China. Ore Geology Reviews 31, 3-47.
Mineral List
32 entries listed. 26 valid minerals.
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