Latitude: 40°47'35"N
Longitude: 110°50'5"E
后石花金矿, 武川县, 呼和浩特市, 内蒙古自治区, 中国
Medium-scale granitoid-related vein-type gold deposit, hosted in chlorite amphibole schist, amphibole plagioclase gneiss and chlorite schist. Host minerals for gold are chalcopyrite and pyrite. Alteration is apparent and includes epidotization, chloritization, sericitization, pyritization and carbonatization. Gold mineralization is believed to be related to the shearing processes of the Archean Wulashan Group of metamorphic rocks.
References
- Jiuhua Xu, Yuling Xie, and Dayi Qian (1998): Metallogeny and mineralization of gold deposits in Daqingshan area, Inner Mongolia. Geology and Prospecting 34(6), 14-20.
- Jiuhua Xu, Yuling Xie, Dayi Qian, Rufu Ding, and Jianping Li (1999): Characteristics of Ore-Forming Fluids of Gold Deposits in Daqingshan District, Inner Mongolia, China. Journal of University of Science and Technology Beijing 6(2).
- Fengjun Nie, Sihong Jiang, Xinxu Su, and Xinliang Wang (2002): Geological features and origin of gold deposits occurring in the Baotou–Bayan Obo district, south-central Inner Mongolia, People’s Republic of China. Ore Geology Reviews 20, 139-169.
Mineral List
27 entries listed. 20 valid minerals.
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