摘要
利用谱元算法数值模拟了不同地表起伏模型下的补偿线性矢量偶极(Compensated Linear Vector Dipole,CLVD)源Rg波低谷点的特征及相应的震源深度.结果表明,源区地表存在一定起伏情况下,Rg波低谷点依然存在,低谷点位置反映了源区地表起伏的信息,但与理论值仍有一定偏差.Rg波低谷点受远区地表起伏影响较小.
The characteristics of the spectral null of Rg waves generated by CLVD source and the corresponding source depths are simulated numerically with Spectral Element Method under various fluctuation models. The results indicate that the spectral null of Rg waves still exists under certain conditions, and the location of the spectral null reflects the signatures of the surface fluctuation near the source. However, the depth calculated according to the spectral null still has a certain bias compared with the theoretical value. The fluctuant surface far from the source has little effect on the spectral null.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
2011年第11期2831-2837,共7页
Chinese Journal of Geophysics
基金
军控核查技术项目(513310101)资助
关键词
CLVD源
Rg波
低谷点
谱元算法
地表起伏
CLVD source, Rg waves, Spectral null, Spectral Element Method, Surface fluctuation