中文摘要：

深 subduction 和超离频压力的变态让支持的大陆人的研究不仅在中国的稳固的地球科学的发展，而且提供了一个优秀机会提出板 tectonics 理论。鉴于潜水艇 ducted 外壳的性质， subduction 和碰撞的二种类型分别地在自然被认出了。一方面，外壳的 subduction 发生由于海洋的外壳(和平的类型) 或大陆人外壳(高山的类型) 下溢。在另一方面，大陆人碰撞由弧大陆碰撞(Himalaya 西藏类型) 或大陆大陆碰撞(Dabie-Sulu 类型) 继续。在大陆人动力学的未来学习的关键问题深在大陆人是化学变化和微分发掘 subduction 地区，和到大陆人 subduction 的从海洋的 subduction 的时间空间的转变。

英文摘要：

The studies of continental deep subduction and ultrahigh-pressure metamorphism have not only promoted the development of solid earth science in China, but also provided an excellent opportunity to advance the plate tectonics theory. In view of the nature of subducted crust, two types of subduction and collision have been respectively recognized in nature. On one hand, the crustal subduction occurs due to underflow of either oceanic crust （Pacific type） or continental crust （Alpine type）. On the other hand, the continental collision proceeds by arc-continent collision （Himalaya-Tibet type） or continent-continent collision （Dabie-Sulu type）. The key issues in the future study of continental dynamics are the chemical changes and differential exhumation in continental deep subduction zones, and the temporal-spatial transition from oceanic subduction to continental subduction.