从流体包裹体研究探讨金属矿床成矿条件  

Approach to Ore-Forming Conditions in Light of Ore Fluid Inclusions

作　　者：芮宗瑶[1] 李荫清[1] 王龙生[1] 王义天[1] 

机构地区：[1]中国地质科学院矿产资源研究所,北京100037

出　　处：《矿床地质》2003年第1期13-23,共11页Mineral Deposits

摘　　要：根据作者多年来对流体包裹体的研究成果 ,参考了国内外的研究结论 ,提出了一个新的成矿流体分类方案 ,并评述了我国若干典型金属矿床的研究状况 ,由此探讨了金属矿床的形成机制。Abundant information of ore fluid inclusions or melting inclusions has been collected from many famous metallic deposits in China. On the basis of the authors' studies in combination with related data from home and abroad, the ore fluids are classified into four types, namely mafic-ultramafic magma, granitic magma-volatile component-thermal water, thermal water and normal temperature water. Viscosity, saturability, immiscibility, solubility and some other physicochemical parameters of ore fluids seem to be important constraint factors for the formation of ore deposits. This paper makes an approach to genetic mechanism of some typical metallic deposits in China based on the researches into temperature, pressure, salinity and chemical composition of ore fluid inclusions from these deposits.

关 键 词：地球化学 成矿流体 流体包裹体 成矿条件 金属矿床 形成机制 

分 类 号：P618.2[天文地球—矿床学]