Intrusion-related, fault-controlled, disseminated (1-20 g/t PGE) low sulphide Cu-Ni-bearing PGE deposit, hosted along the contact zone between marbles and a mafic intrusion.
Located about 3 km north of Huili.
References
- Yao, Y., and Viljoen, M.J. (2003): Intrusion-hosted PGE mineralization in the Sichuan Province, China. Goldschmidt Conference Abstracts 2003, A650.
- Wang Denghong, Qu Wenjun, Li Chunjie, Li Jiankang, Fu Deming, Fu Xiaofang, and Zhao Zhigang (2006): Geological and Geochemical Features of the Dayanzi Pt-Pd Deposit, Huili, Sichuan and Its Implication for Prospecting. Geological Review 52(2), 219-223.
- Liguo Guo, Yuping Liu, Wenchao Su, Guofu Zhou, Lin Ye, and Wei Xu (2006): Characteristics of Low Temperature PGE-Mineralization in Dayanzi, Sichuan Province, China: Evidence form BSE and ES Microanalysis. Acta Mineralogica Sinica [Kuangwu Xuebao] 26(2), 203-209.
- Hangxin Cheng, Chuandong Zhao, Guangmin Zhuang, Yinhan Liu, Haifeng Nie, and Lu Qi (2007): Primary geochemical anomaly and blind ore prospecting in the Dayanzi Pt-Pd deposit, Sichuan Province. Geology and Prospecting 43(4), 56-60.
Mineral List
19 entries listed. 16 valid minerals.
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