河南省卢氏县郭家岭金矿地质特征及找矿标志  

Geological characteristics and prospecting indications of Guojialing gold deposit in Lushi county, Henan province

作　　者：张红亮[1] 李佩[1] 张杰[1] 牛宇航 渠玉冰 ZHANG Hong-liang;LI Pei;ZHANG Jie;NIU Yu-hang;QU Yu-bing(The Fourth Geological Exploration Institute of Provincial Bureau of Geo-Exploration and Mineral Development,Zhengzhou 450001,China)

机构地区：[1]河南省地质矿产勘查开发局第四地质勘查院

出　　处：《世界有色金属》2019年第6期213-215,共3页World Nonferrous Metals

基　　金：2014年度河南省地质勘查基金项目(豫国土资发﹝2015﹞96号,项目序号17)

摘　　要：郭家岭金矿位于华北陆块南缘多金属成矿带,矿体赋存于黑沟—栾川断裂的次级断裂中,矿体受北西西向断裂控制,矿化不均匀,矿体呈豆荚状、透镜状。矿化蚀变类型简单,主要为黄铁矿化、褐铁矿化及硅化。初步总结了成矿规律和找矿标志,对今后的勘查工作提出了建议。The Guojialing gold deposit is located in the polymetallic metallogenic belt on the southern margin of the North China continental block. The ore body is located in the secondary fault of the Heigou-Luanchuan fault. The ore body is controlled by NWW fault and the mineralization is uneven. the ore body is pod-shaped and lenticular. The type of mineralization alteration is simple, mainly pyrite mineralization, limonite mineralization and silicification. The metallogenic regularity and prospecting indicators were preliminarily summarized, and suggestions for future exploration work were put forward.

关 键 词：卢氏县 郭家岭金矿 地质特征 找矿标志 

分 类 号：P694[天文地球—地质学]