摘要
本文以含矿地层的构造解折为基础，讨论了胡—篦型铜矿的成矿地质条件，认为矿床成因是多种因素控制下的热液矿床。
Based on the structural analysis of the copper-bearing formation,the geological factors of mineralization of the Hu--Bi copper deposit have been discused. The cause of formation is a hydrothermal ore deposit controlled by same factors.
出处
《西南工学院学报》
1997年第2期60-63,共4页
Journal of Southwest China Institute of Technology
关键词
山西
铜矿床
成矿地质条件
矿床成因
Shanxi Zhongtiao Mountains
Copper ore deposit
Geological factor
Cause
