Located on the northern margin of the Central Tianshan block and south of the Shaquanzi fault, which separates the former from the Jueluotage Late Palaeozoic fold belt. The deposits in this area belong to the conduit type magmatic mineralization. They were discovered in 2002, are situated close to each another and share similar features. At present, they are still being evaluated.
References
- Jingwen Mao, Pirajno, F., Zuoheng Zang, Fengmei Chai, Hua Wu, Shiping Chen, Linsong Cheng, Jianmin Yang, and Changqing Zhang (2007): A review of the Cu-Ni sulphide deposits in the Chinese Tianshan and Altay orogens (Xinjiang Autonomous Region, NW China): Principal characteristics and ore-forming processes. Journal of Asian Earth Sciences (in press).
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