中国造山带研究的回顾和展望

本文简要回顾了20世纪50年代以来中国地质学家在研究显生宙陆（板）缘造山带或古大陆边缘造山带中所取得的进展：多数巨型造山系经历了多阶段古洋盆形成和消亡，陆块碰撞演化历史；离散大陆边缘多样性；洋盆产出环境和消减 迁移多样性。近20年来我国学者加强了造山带三维变形运动学研究，提出了多层次滑脱叠置构造，剖面上、平面上的楔入构造等重要新认识。最后指出中国大陆造山带今后研究热点和展望。

Study of Orogenic Belts in China: Retrospects and Prospects

In this paper, the progress in the study of Phanerozoic plate (contiental)-margin or paleocontinental-margin orogenic belts of China by Chinese geologists since 1949, especially since the 1980's, is reviewed. For example, three tectonic domains have been distinguished in China (i. e. Paleo-Asian, Tethys, circum-Pacific); most gigantic orogenic systems have experienced multi-stage formation and elimination of ancient oceanic basins and continental collision; the diversity of divergent continental margins and that of the environemnt,subduction and migration of oceanic basins have been recognized. In the last two decades, Chinese geologists have strengthened the kinematic study of the three-dimensional deformation of orogenic belts and proposed such new views as multi-layered detachment and superimposion and 3-D wedging. Finally, some hot topics and prospects for further research on continental orogens of China are proposed.