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在野外地质调查研究基础上,总结该矿床矿化富集规律,详细研究矿石硫同位素组成,单矿物包体成分、测温和微量元素等特点,并与国内外一些矿床进行对比,分析探讨矿床的成因,认为该矿床以岩浆热液成因为主,并具有层控矿床某些特点的中偏高温热液矿床。据本区大地构造特征及矿化富集规律,分析了该矿床形成过程,指出了找矿方向的要点。
Based on the field geological survey and research, the mineralization enrichment law of this deposit is summarized, the characteristics of sulfur isotopic composition, single mineral inclusions, temperature and trace elements of ore are studied in detail, compared with some domestic and foreign deposits, The reason is that the deposit is dominated by magmatic hydrothermal origin and is characterized by medium-high temperature hydrothermal deposits with some characteristics of stratabound ore deposit. According to the geotectonic features and mineralization enrichment laws in this area, the forming process of the deposit is analyzed and the main points of prospecting direction are pointed out.