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成矿流体及成矿机制
引用本文:何知礼,杜加锋.成矿流体及成矿机制[J].地学前缘,1996,3(4):0-0.
作者姓名:何知礼  杜加锋
作者单位:[1]北京科技大学 [2]冶金工业部第一地质勘查局
摘    要:近十几年来,流体包裹体(FI)研究有重大进展,尤其在单个FI成分分析方面。激光拉曼微探针、扫描质子微探针(PIXE)和同步加速器X-射线荧光分析(XRF)及一些质谱测定法的应用与发展,能较精确地测定单个FI成分。已有可能对FI中最重要的参数——重金属元素进行较精确测定。这些成就加上超微矿物学等方面的进展,可为解决矿床成因、找矿标志和成矿规律及找矿勘探提供可靠资料。叙述了一些国家在FI研究方面的进展与发展趋势。

关 键 词:流体包裹体  研究进展  发展趋势

SOME ADVANCES AND TRENDS IN FLUID INCLUSION RESEARCH
He Zhili.SOME ADVANCES AND TRENDS IN FLUID INCLUSION RESEARCH[J].Earth Science Frontiers,1996,3(4):0-0.
Authors:He Zhili
Abstract:In recent ten years the research of fluid inclusion has made great progress, especially in the analysis of individual fluid inclusion. The application and improvement of Laser Raman microprobe, Scanning Proton microprobe, and synchrotron X ray fluorecence analysis (XRF) as well as some Mass Spectrometric determinations have enabled us to precisely determine the contents of individual fluid inclusion. And now it is possible to precisely determine the most important parameter in fluid inclusion the heavy metal elements. These advances as well as the progress in ultramicromineralogy can provide us more reliable information about the genesis of ore deposit, prospecting criteria, mineralization regularity and prospecting and exploration. Also this passage gives some information about the progress and trends of some countries in the research of fluid inclusion.
Keywords:fluid inclusion  research progress  research trends  
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