Affiliation:
1. Advanced Data Solutions, 3050 Post Oak Blvd., Ste. 1300, Houston, Texas 77056.
Abstract
Equivalent‐offset migration is a methodology for prestack‐Kirchhoff time migration that partially reverses the order of velocity analysis, normal moveout correction, stack, and migration. Though claimed to be computationally and analytically superior to earlier time‐domain approaches, it is not independent of velocity. Velocity‐independent dip moveout followed by prestack imaging is similar to equivalent‐offset migration in that it also postpones normal moveout correction to the postmigration stage, but it is independent of velocity. This paper investigates the theoretical relationship between these two processes, showing that equivalent‐offset migration and prestack imaging are asymptotically equivalent. Moreover, equivalent‐offset migration has little, if any, computational or analytic advantage. The fact that the combination of dip moveout followed by prestack imaging is independent of velocity is a major advantage and suggests that this latter method is better suited to problems of velocity estimation.
Publisher
Society of Exploration Geophysicists
Subject
Geochemistry and Petrology,Geophysics
Reference19 articles.
1. Transformation to zero offset for mode‐converted waves
2. Transformation to zero offset for mode‐converted waves
3. Anderson, J. E., and Tsvankin, I., 1994, Dip‐moveout processing by Fourier transform in anisotropic media: 64th Ann. Internat. Mtg., Soc. Expl. Geophys., Expanded Abstracts, 1213–1216.
4. Anderson, J. E., Alkhalifah, T. A., and Tsvankin, I., 1994, Fowler DMO and time migration in transversely isotropic media: 64th Ann. Internat. Mtg., Soc. Expl. Geophys., Expanded Abstracts, 1217–1220.
5. Bancroft, J. C., 1997, A Review of migration fundamentals,inHanson, D., Ed., Topics in depth imaging: Proc. 1997 Spring Symp. Geophysical Soc. of Tulsa.
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