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不同的大地构造域在成矿作用方面的差异表现为各大地构造域内部所产出金属矿床种类的不同(de Wit and Thiart,2005)。成矿省反映了地壳的区域地球化学不均一性,其证据表现为各个成矿省所具有的独特“成矿指纹”。根据成矿元素的地球化学亲和性,将其分归类为6组(即:Au、Cr-Ni-PGE-Ti、Cu-Pb-Zn-Ba、Sn-Sb、W、U-Th-REE)进行统计分析。大陆地壳各构造域的“成矿指纹”可以通过上
The differences in mineralization between different tectonic tectonics are characterized by differences in the types of metallogenic deposits produced within each major tectonic domain (de Wit and Thiart, 2005). The metallogenic province reflects the regional geochemical heterogeneity of the crust, and its evidence shows the unique “metallogenic fingerprint” of each metallogenic province. According to the geochemical affinity of the metallogenic elements, they are classified into six groups (ie Au, Cr-Ni-PGE-Ti, Cu-Pb-Zn-Ba, Sn-Sb, W, U-Th- REE) for statistical analysis. The continental “continental crust” tectonic domain “mineralization fingerprint ” can pass on