Hydrothermal Cu deposit, hosted along the Yiche syncline in the contact zone between Emeishan flood basalts and overlying Upper Permian coal-bearing clastic rocks of the Xuanwei formation.
Ref.:
- Zhu Bingquan, Hu Yaoguo, Zhang Zhengwei, Cui Xuejun, Dai Tongmo, Chen Guanghao, Peng Jianhua, Sun Yongge, Liu Dehan, and Chang Xiangyang (2007): Geochemistry and geochronology of native copper mineralization related to the Emeishan flood basalts, Yunnan Province, China. Ore Geology Reviews 32, 366-380.
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