摘要
金矿床中热液流体成矿作用作为一种半开放—开放体系 ,其过程是由多种因素相互耦合的 .这些耦合作用包括含金成矿热液流体体系与控矿环境之间的耦合作用 ,含金成矿流体体系中内素的耦合作用 ,外部环境和各个控矿条件的耦合作用 .其中外部的控矿环境与含金成矿热液流体的耦合程度决定了矿床的形成与否 .
Gold metallogeric process,in a semi open to open ore fluid system, covers a series of coupling processes including those between hydrothermal ore fluid system and ore controlling circumstance, between the internal factors of hydrothermal ore fluid system, and between external environment and each ore controlling condition, of which the coupling level between hydrothermal ore fluid system and ore controlling circumstance decides whether a gold deposit forms
出处
《地质与资源》
CAS
2001年第1期46-49,共4页
Geology and Resources
