Latitude: 42°16'N
Longitude: 124°55'E
线金厂金矿, 清原满族自治县, 抚顺市, 辽宁省, 中国
Large-scale gold deposit, hosted in Archean granulite, hypersthene granite and tonalite that are intruded by the NE-trending Mesozoic Zhuanxianghu quartz diorite. The deposit consists of gold-bearing quartz veins controlled by faults. There are two types of ore bodies, quartz-pyrite and quartz-base metallic sulphide types, and four stages of mineralization, namely (1) quarz vein, (2) base metallic sulphides, (3) fine galena and (4) micro-veinlets. The deposit is interpreted as a magmatic-hydrothermal deposit formed during the Mesozoic.
References
- Pengren Yan (1992): Geochemical features and prognostication criteria for finding magmatic-hydrothermal gold deposits in the Qingyuan area, Liaoning Province. Geology and Prospecting 28(7), 49-53.
Mineral List
21 entries listed. 13 valid minerals.
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