摘要
介绍了中条山郭家沟矿区的地质概况,分析了该矿区的地质特征,从铜凹组一段地层上部矿化与铜凹组二段地层矿化两方面,阐述了矿区的矿化特点,指出该矿区矿化基本属于"层控"现象,后期的石英方解石脉对矿化有进一步富集作用。
This paper introduced the geology situation of Zhongtiaoshan Guojiagou mining area,analyzed the geological characteristics of the mine,from the copper concave group 1 section stratum upper ore potentiality and copper concave group 2 section stratum ore potentiality two aspects,elaborated the ore potentiality characteristics of the mining area,pointed out that the ore potentiality basic attributes belonged to＂stratabound＂phenomenon,the late quartz calcite had further enrichment to ore potentiality.
出处
《山西建筑》
2016年第24期85-86,共2页
Shanxi Architecture
关键词
矿区
铜凹组
矿化特点
地质特征
mining area
copper concave group
mineralization characteristic
geological characteristic
