摘要
河南焦园断裂是区域导矿构造带之一。该断裂主要由压性角砾岩、碎裂蚀变岩组成,反映出带内热液活动强烈。笔者在工作中发现断裂带在柿树底至西凹段具有明显矿化富集特征,也是区内主要找矿靶区之一。
Jiaoyuan fault is one of the regional passages of the ore fluid. It is mainly made of breccias and fragments of altered rocks, which indicates that the hydrothermal activity is strongly developed within the fault zone. The authors found this fault zone is of significant mineralization from Shishudi to the Xi＇ ao. It is one of the main prospecting targets in the region.
出处
《地质调查与研究》
2012年第1期63-66,73,共5页
Geological Survey and Research
关键词
焦园断裂
柿树底
蚀变岩
金矿
河南嵩县
Jiaoyuan fault
Shishudi
altered rock
gold deposit
Songxian County
Henan Province
