深部流体及其与成矿成藏关系研究现状  

Mantle-derived Fluids in Relation to Ore-forming and Oil-forming Processes

作　　者：毛景文[1] 李晓峰[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》2004年第4期520-532,共13页Mineral Deposits

基　　金：国家重点基础研究规划项目"大规模成矿作用与大型矿集区"(编号:G1999043211)的资助

摘　　要：深部流体(地幔流体)及其成岩成矿作用的研究是当今地质科学研究的前沿领域,最近几年这方面的研究进展较快。文章比较详细地讨论了地幔流体的组成、地幔流体中碳氧、氢氧和稀有气体同位素特征、地幔流体类型和运移形式,以及地幔流体活动的构造背景,并对地幔流体与金属矿床、油气田盆地等成矿成藏作用关系的研究现状进行了介绍。The researches on mantle_derived fluids in relation to ore_forming and oil_forming processes constitute one of the forefront fields in the earth science. Based on the research results of this fields in combination with the achievements of the project “Deep Fluids Ore_forming System' supported by the Major State Basic Research Programs of People's Republic of China, this paper has reviewed the compositions, types and migration forms of mantle_derived fluids, discussed O, H, C and noble gas isotopes of mantle_derived fluids and proposed the origins of mantle_derived fluids and its tectonic setting in the active areas. The current researches on the relationships of mantle_derived fluids to the formation of metallic deposits and oil_gas field basins are also reported in this paper.

关 键 词：地质学 地幔流体 油气藏 金属矿床 稀有气体同位素 稳定同位素 综述 

分 类 号：P61[天文地球—矿床学]