Skarn and magmatic hydrothermal type Pb-Zn-W-Mo-Ag deposit, hosted by carboniferous sedimentary rocks around small jurassic plugs of felsic porphyries.
Located near Guiyang, about 45 km west of Chenzhou.
Ref.:
- Xiang-Ping, G., Watanabe, M., Hoshino, K., and Shibata, Y. (2001): Mineral chemistry and associations of Bi-Te(S,Se) minerals from China. Neues Jahrbuch für Mineralogie, Monatshefte, 289-309.
- Shunso Ishihara, Ping'An Wang, Yoshimichi Kajiwara, and Yasushi Watanabe (2003): Origin of sulfur in some magmatic-hydrothermal ore deposits of South China. Bulletin of the Geological Survey of Japan 54(3/4), 161-169.
- Junming Yao, Renmin Hua, Wenjun Qu, Huawen Qi, Jinfu Lin, and Andao Du (2007): Re-Os isotope dating of molybdenites in the Huangshaping Pb-Zn-W-Mo polymetallic deposit, Hunan Province, South China and its geological significance. Science in China, Series D (Earth Sciences), 50(4), 519-526.
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Map Reference: 25°42'N , 112°41'E
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