摘要
铜厂铜矿田位于我国著名的勉略阳地区中 ,是重要的铜金多金属矿田。在将矿床 (化 )类型系统划分为三大类 6个亚类基础上 ,详述了各类型矿床 (化 )的地质特征 ,讨论了其矿床成因。认为铜厂矿田矿床为同位多期—多矿化阶段—多来源的多因复成矿床。
Tongchang orefield is a famous one of that is consists of imprtant polymetal sulfid deposits in the Mian County-Lueyang-Yangpingguan Area ,China. On basis of dividing deposit (mineralization) types systematically, geological characteristics of major deposits have been expatiated ,and deposit genesis has been discussed in this paper. It is thought that deposits in the Tongchang orefield are composite type deposits of parity,poly-period, poly-stage, poly-soure and poly-genesis.
出处
《地质与勘探》
CAS
CSCD
北大核心
2000年第4期11-15,40,共6页
Geology and Exploration
基金
云南省中青年学术和技术带头人培养经费
中日合作项目和中国有色金属工业总公司基金项目
关键词
多因复成成因
铜厂矿田
矿床类型
铜矿床
deposit types,composite deposit of polygenesis,Tongchang orefield,Mian county-Lueyang-Yangpingguan area
