摘要
武山铜矿是长江中下游铁、铜、金成矿带一个重要组成部分 ,通过对武山铜矿北矿带的成因矿物学研究 ,可将其划分为沉积成因系列与热液成因系列两大类 ,从而进一步证明武山铜矿北矿带为在正常沉积基础上 ,由燕山期岩浆热液叠加改造的层控矿床。
Wushan copper deposit is an important part of .Fe. Cu and Au metallogenetic belt in the middle and lower reaches of the Yangtze River. Through research genetic mineralogy of pyrite for North ore zone of Wushan copper deposit, its pyrites might be divided into the sedimentary series and the hydrothermal series. It is a stratabound deposit which formed on the basis of ordinary sedimentary formation and was superimposed and changed by Yanshan ore-bearing magma hydrothermal solution.
出处
《地质与勘探》
CAS
CSCD
北大核心
2002年第5期44-48,共5页
Geology and Exploration
