Medium-scale alkaline complex-hosted altered rock type gold deposit, consisting of varied shaped veins in places where the lower part of the Archean Wulashan Group and Caledonian quartz diorite are widely exposed.
Ref.:
- 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.
- Nie, F.-J., Jiang, S.-H., and Liu Y. (2004): Intrusion-Related Gold Deposits of North China Craton, People's Republic of China. Resource Geology 54(3), 299-324.
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http://wrgis.wr.usgs.gov/open-file/of03-220/DATABASE/lode_deposits.txt22 entries listed. 18 valid minerals.
