Method for compensating 3D DMO for the effects of an inhomogeneo

Communications – electrical: acoustic wave systems and devices – Seismic prospecting – Land-reflection type

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367 52, G01V 136

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052854221

ABSTRACT:
A three dimensional residual modeling operator is applied to seismic times that have been preprocessed by application of NMO and velocity independent DMO. The residual operator compensates for vertical velocity variation and anisotropy and its use precludes the need for ray tracing.

REFERENCES:
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Berg, L. E., "Prestack Partial Migration," 54th Ann Mtg SEG, Atlanta (1984), Reprint by Geophysical Co. of Norway A.S.
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Deregowski et al., "Geometrical Optics & Wave Theory of Constant Offset Sections in Layered Media," Geophysical Prospecting, V. 29, pp. 374-406, (1981).
Gonzales, Alfonso; Levin, Chambers, Ronald E. Franklyn K.; and Mobley, Everett, (1992) A Method of Correcting 3-D DMO for the Effects of Wave Propagation in an Inhomogeneous Earth: 62nd SEG Ann. Internat. Meeting, New Orleans, Oct. 25-29, Expanded Abstracts, 966-969.
Meinardus, Hans A. and Schleicher, Karl, 3-D Time-Variant Dip Moveout by the FK Method: 61st SEG Ann. Internat. Meeting, Houston, Nov. 10-14, Expanded Abstracts, 1208-1210. (1991).
Perkins, Wesley T. and French, William S., 3-D Migration to Zero Offset for a Constant Velocity Gradient: 60th SEG Ann. Internat. Meeting, San Francisco, Sep. 23-27, Expanded Abstracts, 1354-1357.
Dietrich, Michel and Cohen, Jack K., 3-D Migration to Zero Offset for a Constant Velocity Gradient: An analytical Formulation, Geophysical Prospecting (Jan. 1992).
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