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详细的地球物理与区域成矿学的研究,揭示了秦岭地区中生代矿床分布与壳幔深部结构的关系。东秦岭中生代矿床随着远离鲁山深断裂带矿化强度减弱。东、西秦岭矿床类型的差别与壳-幔流变调整作用的强度有关。秦岭地区的立交桥式三维结构对矿床分布,尤其是超大型中生代内生矿床的分布有明显制约。
Detailed geophysical and regional mineralization studies reveal the relationship between the distribution of the Mesozoic deposits and the deep crust and mantle in the Qinling area. The mineralization intensity of the East Qinling Mesozoic ore deposit weakened away from Lushan deep fault zone. The differences between the East Qinling and West Qinling deposits are related to the strength of the adjustment of crust-mantle rheology. The overpass type three-dimensional structure in the Qinling area has obvious constraints on the distribution of the ore deposits, especially the distribution of the super-large Mesozoic endogenic deposits.