【摘要】 本文是作者受国际大地测量和地球物理联合会中国国家委员会的委托，为１９９５年第２１届ＩＵＧＧ大会编写的中国国家报告．报告涉及了１９９１－１９９４年期间中国在大陆岩石圈结构和动力学研究领域内的主要活动和所取得的重要成就，以及各种深部地球物理探测手段在岩石圈研究中的进展情况．将中国大陆岩石圈以南北构造带为界划分为东、西两大部分，在每一部分内又进一步划分出不同的区或带，并较详细地论述了这些区和带的岩石回结构特征．在此基础上，结合地质学的某些主要研究成果，重点探讨了中国东部大陆岩石圈演化和动力学过程．更多还原

【Abstract】 Chinese National Committee for IUGG has entrusted author to write China National Report on the Lithospheric Structure and Dynamics of China for the XXIth General Assembly of IUGG, Colorado, July, 1995. The report has dealt with both the main activities and achievements in reseach field on the lithospheric structure and dynamics and important progress in the geophysical investigations for lithospheric structures in China. In this papet the continent of China is divided into the western part and the eastern part with a dividing boundqry NorthSouth trending tectonic belt situated between 101° and 106°(from south to north) and each part is further subdivided into the different subregions or zones according to the lithospheric structures which are describde in detail for the subregions and zones. THe lithospheric evolution and dynamics of the eastern part of China continent are suggested in this work, however the lithospheric structure and dynamics of the Tibetan plateau are excepted because they are reported by prof.Zeng Rong-Sheng in other paper.更多还原