摘要
本文介绍了一种将断层参数引入到有限元计算的方法——分割结点技术。利用分割结点技术,可以很方便地将断层参数以边界约束的形式引入到有限元的正演解算中。本文首次利用1012个地应力主方向观测数据和中国两期GPSA级网基线观测数据,联合反演了中国及其邻区的三个主要的断层运动参数。
The “Split Node Technique” which can be used in the finite element computations were outlined in the paper. The technique is used to deal with the displacement discontinuity between the two elements. The fault parameters can be introduced as fictitious forces on the nodes adjacent to the split node by using this technique. 1 012 stress orientation observations and two epochs of Chinese A order GPS baseline results were occupied to inverse the parameters of fault movements of three principal fault over the areas of Chinese region and its vicinity.
出处
《测绘学报》
EI
CSCD
北大核心
1998年第2期125-130,共6页
Acta Geodaetica et Cartographica Sinica
关键词
分割结点
断层
有限元
断层反演
Split node, Inversion, Fault, Finite element