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碰撞造山成矿作用研究是矿床学研究与板块构造理论相结合的必然。近三十年来,矿床领域的研究热点和重大进展多与板块理论的应用有关,其中的斑岩铜矿模式是在俯冲体制的地质作用研究取得突破之后不久提出的,并且掀起了至今常盛不衰的环太平洋找矿热潮。相对而言,对碰撞体制的地质作用研究起步较晚,认识程度较低,因而限制了碰撞体制的成矿作用及有关问题的研究,使得至今尚不清楚碰撞体制的成矿规律及有关地质作用的特征。
Collision orogeny mineralization research is the inevitable combination of deposit study and tectonic theory. In recent three decades, the research hot spots and major progress in the field of deposit have been mostly related to the application of plate theory. The model of the porphyry copper deposit was put forward shortly after breakthroughs in the study of the geological function of the subduction system were made, Bad ring of the Pacific ore prospecting boom. Relatively speaking, the study on the geologic mechanism of collision system started relatively late and has a low level of understanding, which limits the metallogenetic effects of the collision system and the related issues, so that it is still not clear about the metallogenic regularity and the related geological effects of the collision system Characteristics.