摘要
文中简要介绍了银山铜多金属矿床的成矿地质背景和矿床地质特征。论述了矿床与本区岩浆活动在时间、空间和成矿物质来源等方面的关系，提出了银山铜多金属矿床是与燕山早期岩浆活动有关的火山—次火山岩浆热液矿床的新认识。
： This paper deals briefly with the geologic setting and geologic features of the Yinshan copper－polymetal deposit, which is closely related, both in space and in time, with magmatic activity that served as a source of ore component for the deposit． The author re－defines the deposit as a volcanic－subvolcanic hydrothermal deposit related with Early Yanshanian magmatism．
出处
《江西地质》
2001年第2期102-106,共5页
Jiangxi Geology
