Latitude: 43°8'10"N
Longitude: 124°35'11"E
山门(四平)银(金)矿, 梨树县, 四平市, 吉林省, 中国
Polymetallic Ag-(Au-Pb-Zn-Cu-Ba) volcanic-hosted metasomatite, consisting of veins, lenses and stockworks. The main part of the deposit is 1800 m long. The deposit minerals occur in masses, veinlets and disseminations. The host rocks are Cambrian and Ordovician intermediate siliceous volcanic rocks, sedimentary clastic and carbonate rocks, that are intruded by Jurassic and Cretaceous granitoids. The deposit is controlled by north- to northeast-trending faults and fracture zones.
References
- Shujuan Sun (1992): The characteristics of the adjacent wall rocks in the Shanmen silver deposit, Jilin Province. Jilin Geology 11(1), 43-52.
- Liyan Zhang and Jigang Tang (1996): Technical mineralogy of Shanmen silver deposit, Jilin. Geology and Prospecting 32(3), 23-27.
- Dong Zhensheng et al. (1996): Geochemistry of low-temperature independent Ag deposits. In: Tu Guangzhi, Ed.: Low Temperature Geochemistry, Science Press (Beijing), 32-42.
- Shouzhong Feng and Miao Feng (2000): Geological features of Shanmen Ag-Au deposit. Journal of Precious Metallic Geology 9(1).
- Wenbin Huang and Haoche Shen (2006): Isotopic geochemistry evidence for genesis of Shanmen silver deposit, Siping. Geology and Prospecting 42(4), 46-50.
Mineral List
48 entries listed. 36 valid minerals.
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