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.
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.
作者
索勇
王春永
郭方方
Suo Yong;Wang Chunyong;Guo Fangfang(The First Geological Team of Henan Nonferous Metal Geology and Mineral Resources Bureau)
出处
《现代矿业》
CAS
2019年第8期18-20,共3页
Modern Mining
基金
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)
关键词
金矿
地质特征
矿床成因
Gold deposit
Geological characteristics
Deposit genesis
