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本文对铜厂铜矿中石英包裹体特征、黄铁矿热电性和卤素分布特征进行了研究 ,结果表明 ,在矿区 F的高度富集区是铜成矿的有利地段 ,且越靠近矿体 ,其中黄铁矿的热电系数负值越大 (以 N型导电为主 ) ,石英中包裹体数量越多、含盐度越高 ,矿化越好。因此 ,该矿区可以加强包裹体、黄铁矿热电性和卤素分布特征研究并指导找矿和对矿化评价。
In this paper, the characteristics of quartz inclusions, thermoelectric properties and halogen distribution of pyrite in Tongchang Copper Mine are studied. The results show that the highly enriched area F is a favorable area for copper mineralization and the closer to the ore body, Among them, the pyroelectric coefficient of pyrite has a larger negative value (dominated by N-type conductivity), and the more inclusions in quartz, the higher the salinity and the better mineralization. Therefore, the mining area can enhance the study on the thermodynamics and halogen distribution of inclusions, pyrite, and guide ore prospecting and mineralization evaluation.