Tin-polymetallic sulfide deposit in Upper Devonian black shales, consisting of vein-type orebodies in the upper part and stratiform orebodies at the bottom.
Largest deposit in the Dachang orefield.
Ref.:
- Lattanzi, P., Corazza, M., Corsini, F., and Tanelli, G. (1989): Sulfide mineralogy in the polymetallic cassiterite deposits of Dachang, P.R. China. Mineralium Deposita 24(2), 141-147.
- Ming-Hai Cai, Jing-Wen Mao, Ting Liang, and Hui-Lan Huang (2005): Fluid Inclusion Studies of Tongkeng-Changpo Deposit in Dachang Polymetallic Tin Orefield. Mineral Deposits [Kuangchuang Dizhi] 24(3), 228-241.
- Minghai Cai, Ting Liang, Keli Wei, Huiming Huang, Guoqing Liu (2006): Rb-Sr Dating of the No. 92 Orebody of the Tongkeng-Changpo Deposit in the Dachang Tin-Polymetallic Ore Field, Guangxi, and Its Significance. Geology And Mineral Resources of South China 2006(2), 31-36 (in Chinese with English abstract).
- Cai Minghai, Mao Jingwen, Liang Ting, Pirajno, F., and Huang Huilan (2007): The origin of the Tongkeng-Changpo tin deposit, Dachang metal district, Guangxi, China: clues from fluid inclusions and He isotope systematics. Mineralium Deposita 42(6), 613-626.
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Map Reference: 24°56'N , 107°32'E
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