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在地质勘探工作初期阶段,断定矿化的分布深度和剥蚀程度,对预测评价矿床具有首要意义。在应用传统的矿物-地球化学和地质构造准则评价各类矿化的同时,使用研究标型金属矿物——半导体热电性能的方法取得了成效。此方法是基于标型金属矿物的热电性能和成矿作用的物化条件之间已确定的依从关系,特别是金属矿物热电性能的可变性反映出内生矿
In the early stage of geological exploration, it is of primary importance to predict and evaluate the deposit by determining the depth of mineralization and the degree of denudation. While applying the traditional mineral-geochemical and geological tectonics to evaluate various types of mineralization, the effectiveness of the study on the thermoelectric properties of semiconducting metals is studied. This method is based on the established compliance between the thermoelectric properties of the reference metallogenic minerals and the physico-chemical conditions of the mineralization, in particular the variability of the thermoelectric properties of the metallogenic minerals,