现代矿业 ›› 2019, Vol. 35 ›› Issue (08): 18-20.
• 地质·测量 • 上一篇 下一篇
索勇,王春永,郭方方
出版日期:
发布日期:
基金资助:
* 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)。
Suo Yong,Wang Chunyong,Guo Fangfang
Online:
Published:
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。
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.
Key words: Gold deposit, Geological characteristics, Deposit genesis
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, 35(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, 35(08): 18-20.
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