Azimuth moveout for 3-D prestack imaging

被引:50
作者
Biondi, B [1 ]
Fomel, S [1 ]
Chemingui, N [1 ]
机构
[1] Stanford Univ, Dept Geophys, Stanford Explorat Project, Stanford, CA 94305 USA
关键词
D O I
10.1190/1.1444357
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
We introduce a new partial prestack-migration operator called "azimuth moveout" (AMO) that rotates the azimuth and modifies the offset of 3-D prestack data. Followed by partial stacking, AMO can reduce the computational cost of 3-D prestack imaging. We have successfully applied AMO to the partial stacking of a 3-D marine data set over a range of offsets and azimuths. When AMO is included in the partial-stacking procedure, high-frequency steeply dipping energy is better preserved than when conventional partial-stacking methodologies are used. Because the test data set requires 3-D prestack depth migration to handle strong lateral variations in velocity, the results of our tests support the applicability of BMO to prestack depth-imaging problems. AMO is a partial prestack-migration operator defined by chaining a 3-D prestack imaging operator with a 3-D prestack modeling operator. The analytical expression for the AMO impulse response is derived by chaining constant-velocity DMO with its inverse. Equivalently, it can be derived by chaining constant-velocity prestack migration and modeling. Because 3-D prestack data are typically irregularly sampled in the surface coordinates, AMO is naturally applied as an integral operator in the time-space domain. The AMO impulse response is a skewed saddle surface in the time-midpoint space. Its shape depends on the amount of azimuth rotation and offset continuation to be applied to the: data. The shape of the AMO saddle is velocity independent, whereas its spatial aperture is dependent on the minimum velocity. When the azimuth rotation is small (less than or equal to 20 degrees), the AMO impulse response is compact, and its application as an integral operator is inexpensive. Implementing AMO as an integral operator is not straightforward because the AMO saddle may have a strong curvature when it is expressed in the midpoint coordinates. An appropriate transformation of the midpoint axes to regularize the AMO saddle leads to an effective implementation.
引用
收藏
页码:574 / 588
页数:15
相关论文
共 32 条
[1]  
[Anonymous], 1975, Asymptotic Expansions of Integrals
[2]  
BAGAINI C, 1994, 65 ANN INT M SOC EXP, P1549
[3]  
BEVC D, 1992, STANFORD EXPL PROJ, V75, P91
[5]   3-D prestack migration of common-azimuth data [J].
Biondi, B ;
Palacharla, G .
GEOPHYSICS, 1996, 61 (06) :1822-1832
[6]  
Biondi B, 1994, 64 ANN INT M SOC EXP, P1541, DOI [10.1190/1.1822833, DOI 10.1190/1.1822833]
[7]   TRUE-AMPLITUDE IMAGING AND DIP MOVEOUT [J].
BLACK, JL ;
SCHLEICHER, KL ;
ZHANG, L .
GEOPHYSICS, 1993, 58 (01) :47-66
[8]  
BLEISTEIN N, 1990, 60 ANN INT M SOC EXP, P1366
[9]   OFFSET CONTINUATION IN THEORY AND PRACTICE [J].
BOLONDI, G ;
LOINGER, E ;
ROCCA, F .
GEOPHYSICAL PROSPECTING, 1984, 32 (06) :1045-1073
[10]   Regularizing 3-D data sets with DMO [J].
Canning, A ;
Gardner, GHF .
GEOPHYSICS, 1996, 61 (04) :1103-1114