--> ABSTRACT: A Comparison of AVO Behavior after Prestack Time Migration, Prestack Depth Migration, and Prestack Imaging, by James Allen, Carolyn Peddy, Anat Canning, Glen Denyer; #91020 (1995).
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A Comparison of AVO Behavior after Prestack Time Previous HitMigrationNext Hit, Prestack Depth Previous HitMigrationNext Hit, and Prestack Imaging

James Allen, Carolyn Peddy, Anat Canning, Glen Denyer

In the presence of strong lateral Previous HitvelocityNext Hit gradients or structural complexity, prestack depth Previous HitmigrationNext Hit may be required for AVO Previous HitanalysisNext Hit in order to properly image the prospective reflectors. The use of prestack Previous HitmigrationNext Hit for AVO Previous HitanalysisNext Hit presents a conceptual problem in that the Previous HitmigrationNext Hit process collapses seismic energy to the image point where source-receiver locations coincide. This of course removes the dependence of seismic information with angle of incidence. Therefore, prestack Previous HitmigrationNext Hit algorithms used for AVO Previous HitanalysisNext Hit should be specially designed. Until this time, we have compared the AVO results of prestack time Previous HitmigrationNext Hit and prestack depth Previous HitmigrationNext Hit for data with a simple Previous HitvelocityNext Hit structure and for data with a complex Previous HitvelocityNext Hit structure to test the ability of restack depth Previous HitmigrationNext Hit to maintain relative amplitudes. We also tested a Previous HitvelocityNext Hit-independent time-Previous HitmigrationNext Hit approach know as prestack imaging (PSI). The first example is data across a Gulf Coast bright spot that corresponds to a gas-producing sand. Dips in the small fault block containing the bright spot are about 6???. The reflection from the gas sand displays an increase in amplitude with offset. The AVO behavior of the prestack time migrated CMP gathers matches the Zoeppritz ray-trace AVO model derived from the well logs. The prestack depth Previous HitmigrationTop we used is a Kirchhoff routine. A quantitative measure of amplitudes at varying offsets at the target reflection was compared for each gather covering the bright spot for the three processing techniques. The relative amplitudes of the p estack time and depth migrated gathers were similar. The PSI results were also qualitiatively similar, although the algorithm was not specifically designed for relative amplitude preservation. The second comparison was made for a seismic survey crossing a structurally complex zone in the Arkoma Basin of Oklahoma.

AAPG Search and Discovery Article #91020©1995 AAPG Annual Convention, Houston, Texas, May 5-8, 1995