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各种成因类型的内生金属矿床的构造是多种多样的。因此,力求找出矿床的成因特点与其形成的构造环境之间的一般依属关系,是完全可以理解的。我们认为,这种依属关系是真实存在的,而且也是能揭示出来的,如果我们从矿石沉淀系统的相对的构造“张开—闭合”概念出发,相对的构造张开—闭合的程度主要由矿化的形成深度、围岩的物理-力学性质、大地构造状况以及变形的类型和强度来判定。
Endogenous metal deposits of various genetic types are constructed in a variety of ways. Therefore, it is perfectly understandable to seek a general affiliation between the genesis of the deposit and the tectonic setting it forms. In our opinion, this affiliation is real and can be revealed. If we proceed from the concept of “open-closed” relative structure of the ore precipitation system, the relative openness-closure of the structure mainly consists of The depth of mineralization, the physical-mechanical properties of the surrounding rock, the tectonic setting of the earth, and the type and intensity of deformation.