Vein-type W-REE deposit, located in the southern part of the exposed section (19 km2) of the Jurassic Xihuashan biotite-granite.
Ref.:
- Giuliani, G. (1985): Le gisement de tungstène de Xihuashan (Sud Jiangxi, Chine): Relations granites, altérations deutériques-hydrothermales, minéralisations. Mineralium Deposita 20, 107-115 (in French with English abstract).
- Giuliani, G., Li, Y.D., and Sheng, T.F. (1988): Fluid inclusion study of Xihuashan tungsten deposit in the southern Jiangxi province, China. Mineralium Deposita 23, 24-33.
- Yishan Zeng, Yongfeng Zhu, and Jiaqi Liu (2001): Carbonaceous material in S-type Xihuashan granite. Geochemical Journal 35, 145-153.
- Yishan Zeng, Jiaqi Liu, and Yongfeng Zhu (2002): Short-chain carboxylates in high-temperature ore fluids of W-Sn deposits in south China. Geochemical Journal 36, 219-234.
- Orris, G.J., and Grauch, R.I. (2002): Rare Earth Element Mines, Deposits and Occurrences. USGS Open-File Report 02-189, 174 pp.
- 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.
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Map Reference: 25°27'40"N , 114°19'0"E
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