Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
1752880 | International Journal of Coal Geology | 2015 | 28 Pages |
Abstract
Hydrothermal solutions have played a significant role in producing the elemental and mineralogical anomalies in the Lincang Ge ore deposit. The hydrothermal solutions leaching the batholith granite were a mixture of alkaline N2-bearing and volcanogenic CO2-bearing fluids, which led to the enrichment of trace elements, not only including assemblages of Ge-W and Be-Nb-U (both leached from granite and the deposited in the peat), but also As-Sb (from volcanogenic solution), as well as the alteration and argillization of the batholith granites, and the formation of carbonate and quartz-carbonate metasomatites.
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Authors
Shifeng Dai, Peipei Wang, Colin R. Ward, Yuegang Tang, Xiaolin Song, Jianhua Jiang, James C. Hower, Tian Li, Vladimir V. Seredin, Nicola J. Wagner, Yaofa Jiang, Xibo Wang, Jingjing Liu,