Ray tracing in factorized anisotropic inhomogeneous media

50Citations
Citations of this article
16Readers
Mendeley users who have this article in their library.

Abstract

A concept of a factorized anisotropic inhomogeneous (FAI) medium is introduced. In the FAI medium, the position dependent density normalized elastic parameters aijkl(Xi) can be factorized in the following sense: aijkl(Xi) =f2(xi)Aijkl, where Aijkl are constants, independent of Cartesian coordinates xi, and f(xi) is an arbitrary continuous function of xi. Thus, all the density normalized elastic parameters aijkl(xi) in the FAI medium depend on the coordinates xi in the same way, but the generality of anisotropy and of inhomogeneity is not restricted. The factorization of aijkl(xi) leads to a factorization of certain important ray theory expressions and equations (eikonal equation, etc.), and to particularly simple ray tracing and dynamic ray tracing. For certain types of FAI media, these equations may even be solved analytically or semianalytically. Copyright © 1989, Wiley Blackwell. All rights reserved

Cite

CITATION STYLE

APA

Červený, V. (1989). Ray tracing in factorized anisotropic inhomogeneous media. Geophysical Journal International, 99(1), 91–100. https://doi.org/10.1111/j.1365-246X.1989.tb02017.x

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free