摘要
根据银山Ｃｕ－Ａｕ多金属矿床是由构造动力热液和火山－岩浆热液双重耦合成矿作用而形成的新认识，建立了银山矿床新的矿化分带体系──二级多中心矿化分带模式，并探讨了其形成机制及找矿意义。
According to the new recognition that Yinshan Cu-Au polymetallic deposit was formed by double-coupling mineralization between tectonic dynamic hydrothermal solution and volcanic-magmatic hydrothermal solution, the system of mineralization zoning of the deposit, sedond-order and multi-centre mineralization zoning model,was set up, and the mechanism and ore prospecting significance were approached.
出处
《地质与勘探》
CAS
CSCD
北大核心
1996年第5期1-7,共7页
Geology and Exploration
关键词
多金属矿床
矿化分带
成矿作用
铜矿床
金矿床
polymetallic ore deposit,mineralization zoning,mineralization, porphyry,Yinshan in Jangxi
