A physical model of shear‐wave propagation in a transversely isotropic solid-Reference-Cited by-同舟云学术

A physical model of shear‐wave propagation in a transversely isotropic solid

Published:1994-03 Issue:3 Volume:59 Page:484-487
ISSN:0016-8033
Container-title:GEOPHYSICS
language:en
Short-container-title:GEOPHYSICS

Author:

Chang Chih‐Hsiung¹,Gardner G. H. F.²,McDonald John A.³

Affiliation:

1. Allied Geophysical Laboratories, University of Houston, Houston, TX 77204-4231;

2. Dept. of Geology and Geophysics, Rice University, Wiess School of Natural Sciences, P.O. Box 1892, Houston, TX 77251

3. Allied Geophysical Laboratories, University of Houston, Houston, TX 77204-4231

Abstract

It is now understood that seismic anisotropy is a comparatively common phenomenon in sedimentary layers. The elastic properties of most sedimentary rocks have been shown to be anisotropic. (Anisotropy means that the physical property of the material is a function of the measuring direction). Seismologists are generally concerned with velocity variation with the direction of propagation.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Link

https://library.seg.org/doi/pdf/10.1190/1.1443610

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