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锡田矿田位于南岭成矿带中段北缘,区内发育了较大规模的钨锡成矿作用。自2001年以来,研究者们对该区及其临近地区的地质特征、岩体地质地球化学特征、成岩成矿年龄、成矿流体、成矿物质来源、矿床成因类型和成矿规律等做了大量科研生产工作(黄革非等,2001;马铁球等,2004;罗洪文等,2005;杨晓君等,2007;马艳丽等,2008)。在成矿流体方面上,前人未对汇源矿床的流体包裹体进行研究。本文通过对锡田各个期次石英脉中流体包裹体岩相学、显微测温学和激光拉曼光谱分析,
Tin Tin ore field is located in the northern margin of the middle of the Nanling metallogenic belt, the region developed a large-scale tungsten-tin mineralization. Since 2001, the researchers have done a survey on the geological characteristics, geologic and geochemical characteristics of rock mass, age of diagenesis and mineralization, source of ore-forming fluid, type of metallogenic source, type of genesis and metallogenic regularity of the area and its vicinity A large number of scientific research and production work (Huang leather non-equal, 2001; Ma Tieqiu et al., 2004; Luo Hongwen et al., 2005; Yang Xiaojun et al., 2007; In terms of ore-forming fluids, no predecessors have studied the fluid inclusions in Huiyuan deposit. In this paper, the lithofacies, microscopic thermometry and laser Raman spectroscopy of fluid inclusions in various quartz veins of tin field are analyzed.