Geological Characteristics and Genesis of the Womagou Au-Cu Deposit in Qinghai

Proceeding

2020 International Conference of Recent Trends in Environmental Sustainability and Green Technologies

DOI

DOI: https://doi.org/10.48062/978-1-7773850-0-2.005
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Author(s)

Chen Libiao, Chao Haide, Ren Wenkai

Corresponding Author

Chen Libiao

Abstract

The Womagou Au-Cu polymetallic deposit is distributed in the Elashan area of Tibetan Autonomous Prefecture, Qinghai. It is located in the Zhiyi-Tongyugou Cu-Pb-Zn-Sn-Au-Barite IV metallogenic belt on the east side of the East Kunlun metallogenic belt, and is an important polymetallic mineralization area in Qinghai. There are a large number of Cu polymetallic mines in this area, and thus this ore belt has a very important position in China. This area is not only very complex in structure, but also shows the characteristics of multi-cycle evolution, and it belongs to a very important structural knot in west China. Au in the area has a good correlation with Cu and Ag, presenting great mineralization potential. In the future, it is needed to strengthen the prospecting of related Ag deposits in this area.

Keywords

East kunlun metallogenic belt, Qinghai province, Womagou au-cu deposit, Deposit geology, Deposit genesis

Acknowledgments

This research was financially supported by China Geological Survey: “Investigation of Geology and Mineral Resources in Sunan--Dachaidan Area in Qilian Metallogenic Belt”(No. DD20160012)

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