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。
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.
出处
《地学前缘》
EI
CAS
CSCD
1996年第4期306-312,共7页
Earth Science Frontiers
