ARTICLE

A linearized group velocity approach for two-point qP ray tracing in a layered orthorhombic medium

P.F. DALEY E.S. KREBES
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Department of Geoscience, University of Calgary, 2500 University Drive, Northwest Calgary, Alberta, Canada T2N 1N4.,
JSE 2016, 25(1), 87–101;
Submitted: 9 June 2025 | Revised: 9 June 2025 | Accepted: 9 June 2025 | Published: 9 June 2025
© 2025 by the Authors. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution -Noncommercial 4.0 International License (CC-by the license) ( https://creativecommons.org/licenses/by-nc/4.0/ )
Abstract

Daley, P.F. and Krebes, E.S., 2016. A linearized group velocity approach for two-point qP ray tracing in a layered orthorhombic medium. Journal of Seismic Exploration, 25: 87-101. Using a linearized approximation for the quasi-compressional phase velocity, vip in an orthorhombic anisotropic medium, which is a subset of the related quasi-compressional (qP) wave propagation in a general 21 parameter anisotropic medium, a linearized compressional group velocity may be derived as a function of group angles only. In addition, linearized analytic expressions for the components of the slowness vector in terms of group velocities and angles are also obtained. These expressions are used to define two nonlinear equations which are a generalization of Snell’s Law. The solutions of these are used to determine the propagation directions of the reflected and transmitted rays due to an incident ray at an interface between two orthorhombic media. The axes of anisotropy, in both media are, in general, not aligned with the interface separating them. Computer code has been written to consider ray tracing in media defined by a type of large scale 3D finite element blocking (blocky structures). However, a plane parallel layered medium will be used in preliminary investigations. Additionally, in each of these elements (layers) the anisotropic parameters are initially assumed to be constant, although provisions for at least minimal spatial variations of the anisotropic parameters have been considered.

Keywords
orthorhombic media
two-point ray tracing
group velocity
layered anisotropic media
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Journal of Seismic Exploration, Electronic ISSN: 0963-0651 Print ISSN: 0963-0651, Published by AccScience Publishing