摘要
本文对安徽铜陵马山金铜矿的矿体和围岩进行了微量金的分析、用硫和铅同位素的方法探讨了马山金铜矿的成矿机制，初步认为该矿为侵入岩浆热液矿床。
The microgold of ore body and country rock of Cu,Au deposit in Mashan Tonglin,Anhui is analysed by chemistry and the mechanism of mineralizition is concerned with by sulphur isotope and lead isotope. Mashan Cu,Au deposit was primarily considered as invasive magma hydrothermal type deposit.
出处
《华东地质学院学报》
1996年第1期36-41,共6页
Journal of East China Geological Institute
关键词
金矿床
铜矿床
地球化学
microgold
sulphur isotope
lead isotope
magma hydrothermal type deposit
