Latitude: 44°30'30"N
Longitude: 118°56'0"E
白云诺铅锌多金属矿床, 巴林左旗, 赤峰市, 内蒙古自治区, 中国
Large-scale Pb-Zn-(Ag-Cu-W) skarn, located in the central part of the Huanggangliang-Wulanhaote polymetallic belt. The deposit occurs in a secondary anticline of the Sifangcheng-Bayinwula anticlinorium. Northeast-striking faults control the formation and distribution of the deposit and the igneous intrusions. The strata consist of Early Permian low-grade metamorphic rocks and late Jurassic siliceous and intermediate volcanic rocks. The Early Permian strata host most of the deposit; they are composed of sandy slate, carbonate, and pelitic slate, and occur in the central and southeast parts of the associated district. The Yanshannian granitoids consist of granodiorite, granodioritic porphyry, quartz syenite porphyry, and granite porphyry. The deposit occurs mainly in skarn along a contact zone between the granodioritic porphyry and the country rocks.
References
- Jianzhong Feng (1992): The isotopic characteristics of polymetallic deposits from Huanggangliang to Meng'entaolegai, eastern Inner Mongolia. Liaoning Geology 6(2), 117-126.
- Qi Wang and Yongfu Ai (1995): Study on the relationship between Mn-rich Clinopyroxene and Metallization in the Baiyinnuo Pb-Zn Deposit, Inner Mongolia. Acta Scientiarium Naturalium Universitatis Pekinensis 41(2), 224-228.
Mineral List
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