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现代矿业 2019, Vol. 35 Issue (08) :18-20    DOI:
地质·测量 最新目录 | 下期目录 | 过刊浏览 | 高级检索 << Previous Articles | Next Articles >>
豫西申家窑—葫芦峪金多金属矿地质特征及成因
索勇,王春永,郭方方*
河南省有色金属地质矿产局第一地质大队
Geological Features and Genesis of the Shenjiayao-Huluyu Gold Deposit in Western Henan Province
Suo Yong,Wang Chunyong,Guo Fangfang*
The First Geological Team of Henan Nonferous Metal Geology and Mineral Resources Bureau

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摘要 豫西申家窑—葫芦峪金矿区位于崤山金银多金属成矿带上,成矿条件良好。矿区赋矿岩层为太华群岩层,矿区内发育的崤01、崤09等NNW向断裂是重要的控矿、容矿断裂。在阐述申家窑金矿区成矿地质背景、矿体地质特征的基础上,探讨了矿床成因,认为矿床成因类型为构造蚀变岩型金多金属矿。
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索勇
王春永
郭方方
关键词金矿   地质特征   矿床成因     
Abstract: Shenjiayao-Huluyu gold deposit in Western Henan Province is a part of Xiaoshan Ag-Au polymetallic mineralizing belt,the metallogenic condidtions of the area is good.The ore-bearing rock layers of the mining area is mainly for Taihua Group.The important ore-controlling and ore-leading faults of the mining area are mainly for Xiao01 and Xiao09 faults,which direction is NNW.Based on analyzing the metallogenic geological background of the mining area and ore-body geological characteristics,the deposit genesis is discussed.The results show that the deposit genesis is a tectonic alteration rock type Au-polymetallic deposit.
KeywordsGold deposit   Geological characteristics   Deposit genesis     
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* 河南省2011年度地质勘查基金项目(豫国土资发[2013]7号);河南省2014年度地质勘查基金项目(豫国土资发[2015]7号)。

引用本文:   
索勇, 王春永, 郭方方.豫西申家窑—葫芦峪金多金属矿地质特征及成因[J]  现代矿业, 2019,V35(08): 18-20
SUO Yong, WANG Chun-Yong, GUO Fang-Fang.Geological Features and Genesis of the Shenjiayao-Huluyu Gold Deposit in Western Henan Province[J]  Modern Mining, 2019,V35(08): 18-20
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