Citation: | WU Yu, WANG Zhen-qiang, XIA Yan, YUE Tao, XUE Zhi-qiang, SONG Jia-wei. GEOLOGY AND GENESIS OF THE WEIMUSI TUNGSTEN-MANGANESE POLYMETALLIC DEPOSIT IN SONG COUNTY, HENAN PROVINCE[J]. Geology and Resources, 2021, 30(6): 683-689. doi: 10.13686/j.cnki.dzyzy.2021.06.006 |
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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Geological sketch map of Weimusi W-Mn polymetallic orefield
Profile of Weimusi W-Mn polymetallic orefield along No.5 exploratory line
Ore structures of Weimusi W-Mn polymetallic orefield