摘要
本文根据开合观点,将板缘构造与板内构造结合起来,按前震旦纪、古生代和中新生代三个阶段总结了中国板块构造的基本格局。对比各阶段板块构造的特征,得出中国板块构造演化的总体趋势是:板块规模逐渐增大;板内构造愈来愈复杂与多样;板块力学性质表现为刚性不断增强。
In the light of the view of 'Opening and Closing' , in combination with the plate boundary tectonics and the intraplate tectonics, the essential pattern of the plate tectonics of China is summarized in three stages: the Pre-Sinian, the Paleozoic, and the Mesozoic-Cenozoic. A comparison of the plate tectonic features in different stages reveals that the general evolutional trend of the China plate tectonics consists in the increase of plate-size, the complication and variation of the intraplate tectonics and the gradual strengthening of the mechanical rigidity of the plate.
出处
《地球科学（中国地质大学学报）》
EI
CAS
CSCD
北大核心
1991年第5期505-513,共9页
Earth Science-Journal of China University of Geosciences
关键词
板块
构造
中国
plate tectonics, plate movement, 'Opening and Closing' , China.
