An elastic full-waveform inversion based on wave-mode separation

被引:4
作者
Qu, Yingming [1 ]
Li, Jinli [2 ,3 ]
Li, Zhenchun [1 ]
Huang, Jianping [1 ]
机构
[1] China Univ Petr, Sch Geosci, Qingdao 266580, Peoples R China
[2] Chinese Acad Geol Sci, Inst Geophys & Geochem Explorat, Langfang 065000, Peoples R China
[3] Natl Ctr Geol Explorat Technol, Langfang 065000, Peoples R China
基金
美国国家科学基金会;
关键词
elastic full-waveform inversion; encoding multi-source; multi-scale decomposition; P- and S-wave mode separation; step search method in subspace; time-domain; SEISMIC-REFLECTION DATA; REVERSE TIME MIGRATION; LAPLACE-FOURIER-DOMAIN; BOTTOM-CABLE DATA; FREQUENCY-DOMAIN; VTI MEDIA; PART; 2D; STRATEGY; TOMOGRAPHY;
D O I
10.1071/EG16158
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
Multi-parameter elastic full-waveform inversion (EFWI) attempts to find high resolution model parameters that are able to match observed data exactly by minimising residuals between the observed and predicted data. However, the coupling of V-p and V-s, and the cross-talk artefacts between P- and S-wave modes increase non-uniqueness and ill-conditionedness. We propose a new EFWI method based on P- and S-wave mode separation to mitigate these problems. In this method, we derive the gradient formulas with respect to various wave modes using a P- and S-wave mode separated first-order velocity-stress wave equation, and use a step search method in subspace to calculate the corresponding step lengths. The algorithm, called wave-mode separation EFWI (SEFWI), appears to be helpful to weaken non-uniqueness and ill-conditionedness of conventional EFWI by decoupling multiple parameters. Numerical examples conducted with a synthetic dataset modelled on a simple model with anomalies reveal that SEFWI can reduce the cross-talk artefacts between P- and S-wave modes. Synthetic tests on the Marmousi2 model demonstrate that SEFWI yields better inversion results than conventional EFWI. Although the computational cost of SEFWI per iteration is 1.81 times as much as that of EFWI, the total computational cost is almost at the same level, because of its faster convergence rate.
引用
收藏
页码:530 / 552
页数:23
相关论文
共 61 条
[1]  
Aki K., 2002, QUANTITATIVE SEISMOL
[2]   An efficient multiscale method for time-domain waveform tomography [J].
Boonyasiriwat, Chaiwoot ;
Valasek, Paul ;
Routh, Partha ;
Cao, Weiping ;
Schuster, Gerard T. ;
Macy, Brian .
GEOPHYSICS, 2009, 74 (06) :WCC59-WCC68
[3]   Which data residual norm for robust elastic frequency-domain full waveform inversion? [J].
Brossier, Romain ;
Operto, Stephane ;
Virieux, Jean .
GEOPHYSICS, 2010, 75 (03) :R37-R46
[4]   Seismic imaging of complex onshore structures by 2D elastic frequency-domain full-waveform inversion [J].
Brossier, Romain ;
Operto, Stephane ;
Virieux, Jean .
GEOPHYSICS, 2009, 74 (06) :WCC105-WCC118
[5]   MULTISCALE SEISMIC WAVE-FORM INVERSION [J].
BUNKS, C ;
SALECK, FM ;
ZALESKI, S ;
CHAVENT, G .
GEOPHYSICS, 1995, 60 (05) :1457-1473
[6]  
Cheong S., 2004, SEG TECHNICAL PROGRA, P1842
[7]   Efficient calculation of the steepest descent direction for source-independent seismic waveform inversion: An amplitude approach [J].
Choi, YS ;
Shin, C ;
Min, DJ ;
Ha, T .
JOURNAL OF COMPUTATIONAL PHYSICS, 2005, 208 (02) :455-468
[8]  
Choi Y, 2011, GEOPHYSICS, V76, pR125, DOI [10.1190/GEO2010-0210.1, 10.1190/geo2010-0210.1]
[9]   2D Elastic Waveform Inversion in the Laplace Domain [J].
Chung, Wookeen ;
Shin, Changsoo ;
Pyun, Sukjoon .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2010, 100 (06) :3239-3249
[10]   A nonsplit complex frequency-shifted PML based on recursive integration for FDTD modeling of elastic waves [J].
Drossaert, Francis H. ;
Giannopoulos, Antonios .
GEOPHYSICS, 2007, 72 (02) :T9-T17