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通过对铜厂矿区黄铁矿热电系数研究 ,提出可以根据黄铁矿热电系数指导该区铜矿的寻找和评价 ,即黄铁矿热电系数为较大负值、导电型为N型导电的是铜矿赋存地段 ;而黄铁矿导电型为较小负值、导电型为N型或以N型导电为主的是铜矿化有利地段 ;黄铁矿热电系数为较高正值、其导电型为P型或以P型导电为主的地段一般没有矿化。
Based on the study of pyroelectric coefficient of pyrite in Tongchang Mining Area, it is proposed that the thermodynamic coefficient of pyrite should be used to guide the searching and evaluation of the copper deposits in this area. That is, the pyroelectric coefficient of pyrite is larger negative and the conductivity type is N-type conductivity Copper deposits; while the pyrite conductivity type is smaller negative, conductivity type is N-type or N-type conductivity is mainly copper mineralization favorable region; pyrite thermoelectric coefficient is higher positive value, its Conductive P-type or P-type conductivity-based areas are generally not mineralized.