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| GEOLOGY AND GENESIS OF THE WEIMUSI TUNGSTEN-MANGANESE POLYMETALLIC DEPOSIT IN SONG COUNTY, HENAN PROVINCE |
| WU Yu1,2, WANG Zhen-qiang1,2, XIA Yan1,2, YUE Tao1,2, XUE Zhi-qiang1,2, SONG Jia-wei1,2 |
1. No.1 Institute of Geology and Mineral Resources of Henan Provincial Geology and Mineral Exploration and Development Bureau, Luoyang 471000, China;
2. Key Laboratory of Gold-Silver Polymetallic Ore-forming Series and Deep Prediction in Henan Province, Luoyang 471000, China |
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Abstract The Weimusi tungsten-manganese polymetallic deposit in Song County, tectonically located at the junction of Xiong'er Mountain uplift and Songxian fault basin in the eastern section of Huaxiong platform margin depression, is a new type of W-Mn polymetallic deposit discovered in western Henan Province in recent years. The orebodies are occurred in the NW-trending fracture zone on the margin of fault basin, controlled by formation lithology, structure and magmatic hydrothermal fluid. Three W-Mn polymetallic orebodies are delineated, with paragenesis of W, Mn, Pb and Fe. The genesis of deposit is closely related to postmagmatic hydrothermal filling and metasomatism, belonging to the postmagmatic hydrothermal W-Mn polymetallic deposit.
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Received: 18 January 2021
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2021, Vol. 30 
