河南嵩县喂母寺钨锰多金属矿地质特征及成因探讨

doi:10.13686/j.cnki.dzyzy.2021.06.006

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摘要嵩县喂母寺钨锰多金属矿区位于华熊台缘拗陷东段，熊耳山隆起与嵩县断陷盆地的结合部位，为近年来在豫西地区发现的新型钨锰多金属矿床.矿体赋存在断陷盆地边缘的北东向断裂破碎带中，已圈出钨锰多金属矿体3条，钨、锰、铅、铁共生.矿体受地层岩性、构造、岩浆热液等因素控制，矿床成因与岩浆期后热液充填交代作用关系密切，属岩浆期后热液型钨锰多金属矿床.

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	吴煜
	王振强
	夏炎
	岳涛
	薛志强
	宋佳伟

关键词 ：控矿因素, 矿床成因, 钨锰多金属矿, 岩浆期后热液, 河南省

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.

Key words： ore-controlling factor deposit genesis W-Mn polymetallic deposit postmagmatic hydrotherm Henan Province

收稿日期: 2021-01-18

PACS:	P618.32
	P618.67

基金资助:2014年度河南省财政地质勘查基金项目"河南省嵩县喂母寺重晶石铅钨多金属矿普查"（豫国土资发[2015]70号-4）.

作者简介: 吴煜(1986-),男,硕士,工程师,从事区域地质调查及矿产勘查工作,通信地址河南省洛阳市洛龙区开元大道地矿大厦,E-mail//77301329@qq.com

引用本文:

吴煜, 王振强, 夏炎, 岳涛, 薛志强, 宋佳伟. 河南嵩县喂母寺钨锰多金属矿地质特征及成因探讨[J]. 地质与资源, 2021, 30(6): 683-689.
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. GEOLOGY AND RESOURCES, 2021, 30(6): 683-689.

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http://manu25.magtech.com.cn/Jweb_dzyzy/CN/10.13686/j.cnki.dzyzy.2021.06.006 或 http://manu25.magtech.com.cn/Jweb_dzyzy/CN/Y2021/V30/I6/683

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