文章摘要
郭克剑.熊耳山东段祁雨沟金矿区矿源层成因浅析[J].矿产勘查,2019,(5):1075-1081
熊耳山东段祁雨沟金矿区矿源层成因浅析
Origin of ore source bed for Qiyugou Au deposit, Eastern Xiong’ershan region
投稿时间:2018-12-28  
DOI:
中文关键词: 熊耳山  太华群  矿源层  绿岩建造
英文关键词: Xiongershan,Taihuaqun,mine source layer,the construction of the lvyan
基金项目:
作者单位
郭克剑 河南省有色金属矿产探测工程研究中心,郑州 450016
河南省有色金属地质矿产局第二地质大队,郑州 450016 
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中文摘要:
      祁雨沟金矿区处于熊耳山变质核杂岩构造东段,太华群是有利成金的花岗-绿岩建造,是初始矿源层,经长期的构造演化,下迁富集形成衍生矿源层,为该区早白垩世大规模成矿作用提供了物质基础。
英文摘要:
      Qiyugou Au deposit is situated in the eastern section of Xiong’ershan metamorphic core complexes, Taihua group consisting of granite-greenstone formation favorable for gold mineralization serves as an initial ore source bed, and owing to the downward migration enrichment in the course of long term tectonic evolution, the initial source bed transformed into the derivative source bed which is finally responsible for the large scale mineralization occurring in early Cretaceous in the region.
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