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太平洋与亚洲大陆之间的贝尼奥夫带,是控制地槽岩浆活动和成矿作用的纲要性构造.文章阐述了岩浆活动和成矿作用的发展史,以及岩浆矿床与贝尼奥夫带在区域上的空间关系.
The Benioff belt between the Pacific Ocean and the Asian continent is a tectonic structure controlling the magmatism and mineralization of the geosyncline.The paper expounds the history of magmatic activity and mineralization and the relationship between the magmatic deposit and the Benioff belt The spatial relationship in the area.