Medium-sized Zn-Pb-(Ag-Cu-W) skarn, located in the contact zone between Mesozoic granite and Devonian limestone. The orebodies are lenticular and lentoid in shape and vary in scale. Alteration is mainly skarnization. Sn, Bi, Ag and Au in ores are recoverable.
Ref.:
- Ji-Hong Li (2006): Application of the Integrated Multi-Source Geo-Informations and Marginal Mineralization Theory to Ore Prediction-A Case of Polymetallic Ore Prediction in East Ujimqin County, Inner Mongolia, China. Contributions to Geology and Mineral Resources Research [Dizhi Zhaokuang Luncong] 21, 107-112.
- 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.
- http://wrgis.wr.usgs.gov/open-file/of03-220/DATABASE/lode_deposits.txt
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Map Reference: 46°28'47"N , 118°40'0"E
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