Generalized velocity approximation

Author:

Stovas Alexey1ORCID,Fomel Sergey2ORCID

Affiliation:

1. Norwegian University of Science and Technology (NTNU), Department of Geoscience and Petroleum, S. P. Andersens veg 15a, Trondheim 7031, Norway..

2. University of Texas at Austin, John A. and Katherine G. Jackson School of Geosciences, Bureau of Economic Geology, Austin, Texas, USsA..

Abstract

We have developed a new approximation for P-wave velocity that has the same functional form for phase and group velocities. We call it the generalized velocity approximation (GVA) because it is similar to the generalized moveout approximation. The 2D GVA has five parameters, and the 3D GVA has 12 parameters. Our approximation is exact for the phase velocity in a transversely isotropic medium. The parameters of the 3D version of the proposed approximation are defined in all of the symmetry planes in the same fashion. Numerical examples indicate that our approximation has the same accuracy as recently proposed anelliptic approximation, but it has fewer parameters.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference73 articles.

1. Al-Dajani, A., and M. N. Toksoz, 2002, Nonhyperbolic reflection moveout for orthorhombic media: MIT Earth Resources Laboratory Industry Consortia annual report, http://hdl.handle.net/1721.1/67847, accessed 21 December 2011.

2. Nonhyperbolic reflection moveout for azimuthally anisotropic media

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4. Acoustic approximations for processing in transversely isotropic media

5. The offset‐midpoint traveltime pyramid in transversely isotropic media

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