摘要
建立了板内块体的刚性弹塑性运动应变模型 ,并对其进行了块体应变参数唯一性与速度残差中误差最小检验 .根据中国大陆及周围地区的速度场 ,估计了 8个块体的应变参数 ,分析了这些块体的应变状态 .本文估计的各个块体的应变状态与地质学、地球物理学方法估计的结果具有很好的一致性 .由喜马拉雅块体主压应变方向估计的印度板块向欧亚板块碰撞力的主方向为北东 7.
The model of rigid and elastic-plastic motion and strain in intraplate blocks is established in the paper. The unique of strain parameters and minimum root-mean-square error of velocity residual of blocks are tested in the model. Based on the velocity fields in Chinese mainland and its peripheral areas, the strain parameters of 8 blocks are estimated and their strain status analyzed. The estimated strain status of each block is well consistent with those derived by the methods of geology and geophysics. The principal direction of collision force from India plate to Eurasia plate estimated from the azimuth of principal compressive strain of Himalaya block might be N7.1E.
出处
《地震学报》
CSCD
北大核心
2001年第6期565-572,共8页
Acta Seismologica Sinica
基金
国家重点基础研究发展规划项目 (G1 9980 40 7)资助
