摘要
本文将计算合成地震图的广义反射、透射系数矩阵和离散波数方法应用于静态问题,给出了分层介质中位错点源产生的静态位移场的计算方法。该方法保留了反射、透射矩阵方法的原有优点,通过将数值结果与解析解的对比表明,该方法具有较高的数值精度,可用于研究地震断层活动造成的地表形变。
The generalized reflection-transmition coefficient matrix method for calculating synthetc se-ismograms is extended to deal with the static problems,from which a method to calculate the static displacement field of a stratified half space by dislocation source is developed.The advantages of the original reflection-transmition coefficient matrix method are retained.By comparing the numerical results with the analytical solutions,it is shown that this is an effective method for the investigation of the static deformation produced by seismic faulting process.From careful analysis we find there are both similarities and differences between the wave propagation and static problems.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
1989年第3期270-280,共11页
Chinese Journal of Geophysics
基金
国家自然科学基金
关键词
多层介质
位错点源
静态
位移
地震
Stratified half-space
Dislocation source
Static displacement field