Skarn Cu-(Mo) deposit, occurring in the contact zone of porphyries and limestone of the Cretaceous Menzhong Formation. Host rocks are granitic porphyry and quartz porphyry which are fully mineralized.
Ref.:
- Shanyuan Jiang, Zikang Cheng, and Fengjie Han (2006): Geological Characteristics and Potential of Qiangdui Porphyry-Skarn Complex Copper Deposit in Tibet. Contributions to Geology and Mineral Resources Research 21(s), 22-26 (in Chinese with English abstract).
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