SH-SH wave inversion for S-wave velocity and density

被引:12
|
作者
Dai, Fucai [1 ]
Zhang, Feng [1 ]
Li, Xiangyang [1 ,2 ]
机构
[1] China Univ Petr, Beijing 102249, Peoples R China
[2] Lyell Ctr, British Geol Survey, Edinburgh EH14 4AP, Midlothian, Scotland
基金
中国国家自然科学基金;
关键词
MULTICOMPONENT SEISMIC DATA; JOINT PP; RADIATION;
D O I
10.1190/geo2021-0314.1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
SS-waves (SV-SV waves and SH-SH waves) are capable of inverting S-wave velocity (V-S) and density (rho) because they are sensitive to both parameters. SH-SH waves can be separated from multicomponent data sets more effec-tively than the SV-SV wave because the former is decoupled from the PP-wave in isotropic media. In addition, the SH-SH wave can be better modeled than the SV-SV wave in the case of strong velocity/impedance contrast because the SV-SV wave has multicritical angles, some of which can be quite small when velocity/impedance contrast is strong. We derive an approximate equation of the SH-SH wave reflection co-efficient as a function of V-S and rho in natural logarithm variables. The approximation has high accuracy, and it enables the inversion of V-S and rho in a direct manner. Both coefficients corresponding to V-S and rho are "model-parameter in-dependent" and thus there is no need for prior estimate of any model parameter in inversion. Then, we develop an SH-SH wave inversion method and demonstrate it by using synthetic data sets and a real SH-SH wave prestack data set from the west of China. We find that V-S and rho can be reliably estimated from the SH-SH wave of small angles.
引用
收藏
页码:A25 / A32
页数:8
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