2008Geophysical ProspectingRequires access

Slowness surface approximations for qSV‐waves in transversely isotropic media

Alexey Stovas, Y. Roganov

Open publisher page 9 citations

Abstract

ABSTRACT The vertical slowness approximations are widely used in phase‐shift migration methods for quasi P‐ and quasi SV‐waves in transversely isotropic medium. The description of the vertical slowness needed for the migration application for shear waves in transverse isotrophy media is generally complicated. The reason is that this type of approximations results in much simpler expressions for the vertical slowness and, which is most important, they contain fewer parameters than exact expressions. We derive slowness surface approximations valid for qSV‐wave propagation in transversely isotropic and tilted transversely isotropic media by applying an approximation extracted from acoustic approximation for qP‐wave propagation. One approximation has the same accuracy as a qP‐wave acoustic approximation for the same range of horizontal slowness, the other approximations are wide‐angle ones.

About this research paper

What this paper is about

ABSTRACT The vertical slowness approximations are widely used in phase‐shift migration methods for quasi P‐ and quasi SV‐waves in transversely isotropic medium. The description of the vertical slowness needed for the migration application for shear waves in transverse isotrophy media is generally complicated. The reason is that this type of approximations results in much simpler expressions for the vertical slowness and, which is most important, they contain fewer parameters than exact expressions. We derive slowness surface approximations valid for qSV‐wave propagation in transversely isotropic and tilted transversely isotropic media by applying an approximation extracted from acoustic approximation for qP‐wave propagation. One approximation has the same accuracy as a qP‐wave acoustic approximation for the same range of horizontal slowness, the other approximations are wide‐angle ones.

Why it matters

OpenAlex reports 9 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

ABSTRACT The vertical slowness approximations are widely used in phase‐shift migration methods for quasi P‐ and quasi SV‐waves in transversely isotropic medium. The description of the vertical slowness needed for the migration application for shear waves in transverse isotrophy media is generally complicated. The reason is that this type of approximations results in much simpler expressions for the vertical slowness and, which is most important, they contain fewer parameters than exact expressions. We derive slowness surface approximations valid for qSV‐wave propagation in transversely isotropic and tilted transversely isotropic media by applying an approximation extracted from acoustic approximation for qP‐wave propagation. One approximation has the same accuracy as a qP‐wave acoustic approximation for the same range of horizontal slowness, the other approximations are wide‐angle ones.

Key concepts: Slowness, Transverse isotropy, Isotropy, Mathematical analysis, Wave propagation, Physics, Optics, Mathematics

Related papers

Back to paper searchBrowse research topicsOriginal source
Slowness surface approximations for qSV‐waves in transversely isotropic media — Research Paper | ScholarLens