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大陆地壳深俯冲与超高压变质的研究不仅带动了中国固体地球科学的发展,而且为发展板块构造理论提供了契机.根据俯冲地壳的性质,已经认识到俯冲和碰撞分别以两种类型出现.就地壳俯冲来说,存在洋壳俯冲型(例如太平洋周边)和陆壳俯冲型(例如阿尔卑斯造山带).就大陆碰撞来说,则存在弧-陆碰撞型(例如喜马拉雅和青藏造山带)和陆-陆碰撞型(例如大别-苏鲁造山带).大陆俯冲带深部化学变化与差异折返、洋壳俯冲与陆壳俯冲之间的时空转换,将是今后一个时期大陆动力学研究的重点.
The research on the deep crustal subduction and the UHP metamorphism in the continental crust has not only led to the development of solid geoscience in China, but also provided an opportunity for the development of tectonic theory of plate tectonics. According to the nature of subducted crust, it has been recognized that subduction and collision occur in two types respectively For crustal subduction, there are oceanic crust subduction types (such as the Pacific Rim) and continental crust subduction types (such as the Alps orogenic belt). In the case of continental collisions, there are arc-continental collision types (such as the Himalayas and Qinghai-Tibet orogenic belts) (Eg, the Dabie-Sulu orogenic belt), the deep chemical changes and differential reenforcement of the continental subduction zone, and the temporal and spatial transformation between oceanic crust subduction and continental crust subduction will be the focus of continental dynamics research in the coming period.