Beryl-scheelite vein deposit on the southeast slope of the Xuebaoding massif, hosted in intercalating metamorphic rocks and carbonate rocks of the Mid-Triassic Zhagashan Series, and related to an adamellite-monzodiorite intrusion.
Located in the northwest portion of Pingwu county, near the border with Songpan county.
References:
- Guo Yanjun, Wang Rucheng, and Xu Shijin (2000): Vibrational Spectra of Beryl from Xuebaoding, Pingwu County, Sichuan Province. Geological Journal of China Universities 6(2), 201-204.
- Jinhui Lin, Zhimin Cao, Jing Liu, Youguo Li, Yiyun Zhang, and Sancong Ying (2000): Mineral Spectroscopic Studies of Beryls from Xuebaoding, Sichuan. Acta Petrologica et Mineralogica [Yanshikuang Wuxue Zazhi] 19(4), 369-375.
- Cao Zhimin, Zheng Jianbin, Li Youguo, Kabayashi, S., Ren Jianguo, Kaneda, H., Xu Shijin, Shoji, T., and Wang Rucheng (2002): Geologic and geochemical features of the volatile-rich ore fluid and its tracing and dating in the Xuebaoding Beryl-Scheelite Vein Deposit, China. Science in China, Series D (Earth Sciences), 45(8), 719-729.
- Hedland, A. (2004): Das Scheelit-Beryll-Kassiterit-Fluorit-Vorkommen von Huya-Zibeisha bei Pingwu, Provinz Sichuan, China. Mineralien Welt 15 (6), 46-57
- Ottens, B. (2005): Xuebaoding, Pingwu County, Sichuan Province, China. The Mineralogical Record 36(1), 45-57.
- Yan Liu, Jun Deng, Dai-Sheng Sun, and Ying-Hua Zhou (2007): Morphology and Gensis Typomorphism of Minerals in W-Sn-Be Deposit of Huya, Sichuan. Journal of the China University of Geosciences 32(1), 75-81.
