论文部分内容阅读
通过载金矿物黄铁矿热电性研究，得出本区黄铁矿以P型和N－P型导电为主．P型含量高及高的热电系数绝对值指示有利于金矿化，并由此推测可能的有利成矿部位．双王成矿带从西向东，其N型出现率从高到低，反映了从西向东矿体的剥蚀率从大到小，根据黄铁矿热电系数计算得出的热场分布与石准立等（1989）利用含铁白云石中包体均一法测温所得出的温度场相同，对黄铁矿热电性与赋矿围岩之间对应关系及可能原因也进行了讨论。
Through the pyroelectricity study of gold-bearing pyrite, it is concluded that the pyrite in this area is mainly P-type and N-P-type. The P-type high and high pyroelectric coefficient absolute value indication is favorable to gold mineralization, and from this it is possible to speculate the possible favorable metallogenic site. The double-Wang metallogenic belt runs from west to east with high N-type occurrence rate, which reflects the denudation rate from big to small from west to east. Based on pyroelectric coefficient of pyrite, the distribution of thermal field and rock quasi Li et al. (1989) used the same temperature field obtained from the temperature measurement of inclusions in iron-bearing dolomites, and discussed the correspondence between the thermoelectric properties of pyrite and the ore-hosting rocks and the possible reasons for this.