Extraction of amplitude-preserving angle gathers based on vector wavefield reverse-time migration

被引:4
作者
Yang, Jia-Jia [1 ,2 ]
Luan, Xi-Wu [1 ,2 ]
He, Bing-Shou [2 ,3 ]
Fang, Gang [1 ,2 ]
Pan, Jun [1 ,2 ]
Ran, Wei-Min [1 ,3 ]
Jiang, Tao [1 ]
机构
[1] Qingdao Inst Marine Geol, Minist Land & Resources, Key Lab Marine Hydrocarbon Resource & Environm Ge, Qingdao 266071, Peoples R China
[2] Natl Lab Marine Sci & Technol, Funct Lab Marine Mineral Resource Geol & Explorat, Qingdao 266071, Peoples R China
[3] Ocean Univ China, Minist Educ, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266071, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
Elastic wave; reverse-time migration; vector wavefield; angle-domain common-image gathers; amplitude-preserving migration; COMMON-IMAGE GATHERS; POYNTING VECTOR; SEISMIC DATA; S-WAVES; DOMAIN; MEDIA; 2D;
D O I
10.1007/s11770-017-0650-9
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
Angle-domain common-image gathers (ADCIGs) transformed from the shotdomain common-offset gathers are input to migration velocity analysis (MVA) and prestack inversion. ADCIGs are non-illusion prestack inversion gathers, and thus, accurate. We studied the extraction of elastic-wave ADCIGs based on amplitude-preserving elastic-wave reversetime migration for calculating the incidence angle of P-and S-waves at each image point and for different source locations. The P-and S-waves share the same incident angle, namely the incident angle of the source P-waves. The angle of incidence of the source P-wavefield was the difference between the source P-wave propagation angle and the reflector dips. The propagation angle of the source P-waves was obtained from the polarization vector of the decomposed P-waves. The reflectors' normal direction angle was obtained using the complex wavenumber of the stacked reverse-time migration (RTM) images. The ADCIGs of P-and S-waves were obtained by rearranging the common-shot migration gathers based on the incident angle. We used a horizontally layered model, the graben medium model, and part of the Marmousi-II elastic model and field data to test the proposed algorithm. The results suggested that the proposed method can efficiently extract the P-and S-wave ADCIGs of the elastic-wave reverse-time migration, the P-and S-wave incident angle, and the angle-gather amplitude fidelity, and improve the MVA and prestack inversion.
引用
收藏
页码:492 / 504
页数:13
相关论文
共 33 条
[1]  
Aki K., 1980, QUANTITATIVE SEISMOL, P63
[2]  
[Anonymous], 1999, 61 ANN INT C EXH EAG, DOI DOI 10.3997/2214-4609.201407744
[3]  
[Anonymous], 2011, 81 ANN INT M SEG, DOI [10.1190/1.3627847, DOI 10.1190/1.3627847]
[4]   Angle-domain common-image gathers for migration velocity analysis by wavefield-continuation imaging [J].
Biondi, B ;
Symes, WW .
GEOPHYSICS, 2004, 69 (05) :1283-1298
[5]  
Cerveny' V, 2001, SEISMIC RAY THEORY, P17
[6]  
Dickens T.A., 2011, SEG Expanded Abstr, V30, P3109
[7]   Applications of plane-wave destruction filters [J].
Fomel, S .
GEOPHYSICS, 2002, 67 (06) :1946-1960
[8]   REVERSED TIME MIGRATION IN SPATIAL-FREQUENCY DOMAIN [J].
LOEWENTHAL, D ;
MUFTI, IR .
GEOPHYSICS, 1983, 48 (05) :627-635
[9]   MIGRATION BY EXTRAPOLATION OF TIME-DEPENDENT BOUNDARY-VALUES [J].
MCMECHAN, GA .
GEOPHYSICAL PROSPECTING, 1983, 31 (03) :413-420
[10]  
Pinsky M.A., 2009, INTRO FOURIER ANAL W