Latitude: 48°48'N
Longitude: 116°20'E
甲乌拉银铅锌矿, 甲乌拉银多金属矿田, 新巴尔虎右旗, 呼伦贝尔市, 内蒙古自治区, 中国
Polymetallic volcanic-hosted metasomatite, consisting of more than 40 veins that occur along NW-striking fractures. The wallrock is a complicated sequence of Late Permian volcanoclastic rocks of the Laolongto Formation, intermediate to mafic volcanic rocks of the Late Jurassic Tamulangou Formation, intermediate to siliceous volcanic rocks of Late Jurassic Shangkuli Formation, Variscan granite, and Mesozoic diorite porphyry, feldspar, as well as quartz porphyry and beschtauite. Alterations are silica, chlorite, carbonate, sericite, fluorite, epidote, and hydromica. The deposit occurs in a Variscan orogenic belt between the Siberian and North China Platforms.
References
- Daping Wang and Bingcheng Zhu (1992): Geochemical features of fractured structure of the Jiawula deposit. Geology and Prospecting 28(12), 46-52.
- Zhitian Wang, Kezhang Qin, Longju Pang, and Weishi Li (1993): Metallogenic evolution, metallogenic model and exploration model of the Manzhouli-Xin Barag metallogenic province, Inner Mongolia. Mineral Deposits 12(3), 212-220.
Mineral List
27 entries listed. 20 valid minerals.
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