构造动力-火山岩浆同步一体成矿机制——以江西银山金铜多金属矿床为例  

Tectono-Dynamic-Volcano-Magmatic Synchronic Metallogenic Mechanism:an Example from Yinshan Polymetallic Ore Deposit

作　　者：刘丹英[1] 冯志文[1] 张德会[1] 夏卫华[1] 

机构地区：[1]中国地质大学矿产系,武汉430074

出　　处：《地球科学（中国地质大学学报）》1994年第6期815-820,共6页Earth Science-Journal of China University of Geosciences

摘　　要：银山多金属矿床的形成经历了构造动力热液成矿及火山-岩浆热液成矿两个阶段。构造动力热液成矿奠定了银山矿床矿化的基本格局,火山-岩浆热液成矿作用叠加其上,形成了银山大型或特大型金铜多金属矿床。大量事实表明,两种成矿作用在时间上具同期性,构造动力热液成矿稍早些。在空间和成因上两者密切相关,它们构成了构造动力-火山岩浆同步一体的成矿体系。The formation of Yinshan Au-Cu polymetallic ore deposit underwent two metallogenic stages: tectono-dynamic hydrothermal metallization and volcano-magmatic hydrothermal metallization.A lot of geological facts indicate clearly that these two kinds of metallogenesis are basically contemporaneous in time, but the volcano-magmatic metallization is slightly late and it superimposed on the tectono-dynamic metallogenesis. Two kinds of metallogenese are close-ly correlative with each other in space and in origin, they constitute a tectono-dynamic-volcano-magmatic metallogenic system.

关 键 词：成矿体系 多金属矿床 构造动力 火山 岩浆 

分 类 号：P618.205[天文地球—矿床学]