Calculation of phase and groupangles, slowness surfaces and ray tracing in transversely isotropic media

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Autore principale: Karen Pachano Peláez
Natura: Artículo científico
Lingua:en
Pubblicazione: ECOPETROL S.A. 2006
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author Karen Pachano Peláez
author_facet Karen Pachano Peláez
contents Calculation of phase and groupangles, slowness surfaces and ray tracing in transversely isotropic media Karen Pachano Peláez Miguel Duarte Ballesteros Hernando Altamar Mercado Carlos Piedrahita Escobar Trino Salinas Garnica Zuly Calderón Carrillo Ingeniería ray path symmetry isotropy anisotropy elasticity This paper presents some fundamental concepts of seismic anisotropy specifically those which havehexagonal symmetry (ordinarily called transversely isotropic in geophysics jargon).There were made calculations of phase and group angles at a planar interface separating an anisotropicmedia, using routines written in Matlab® and Maple® language. The slowness surfaces of the qP, qSV andSH wave, as well as the ray paths in these two media were also estimated.Although only the simplest situations are discussed, this paper is useful as a first step in understanding thefractured media, because it contains examples, software routines, and a reviewing of the basic concepts andformulas of wave propagation 2006 artículo científico 0122-5383 https://www.redalyc.org/articulo.oa?id=46530203 en http://www.redalyc.org/revista.oa?id=465 CT&F Ciencia, Tecnología y Futuro application/pdf ECOPETROL S.A. CT&F Ciencia, Tecnología y Futuro (Colombia) Num.2 Vol.3
format Artículo científico
id redalyc_46530203
institution Redalyc
language en
publishDate 2006
publisher ECOPETROL S.A.
spellingShingle Calculation of phase and groupangles, slowness surfaces and ray tracing in transversely isotropic media
Karen Pachano Peláez
Ingeniería
ray path
symmetry
isotropy
anisotropy
elasticity
Calculation of phase and groupangles, slowness surfaces and ray tracing in transversely isotropic media Karen Pachano Peláez Miguel Duarte Ballesteros Hernando Altamar Mercado Carlos Piedrahita Escobar Trino Salinas Garnica Zuly Calderón Carrillo Ingeniería ray path symmetry isotropy anisotropy elasticity This paper presents some fundamental concepts of seismic anisotropy specifically those which havehexagonal symmetry (ordinarily called transversely isotropic in geophysics jargon).There were made calculations of phase and group angles at a planar interface separating an anisotropicmedia, using routines written in Matlab® and Maple® language. The slowness surfaces of the qP, qSV andSH wave, as well as the ray paths in these two media were also estimated.Although only the simplest situations are discussed, this paper is useful as a first step in understanding thefractured media, because it contains examples, software routines, and a reviewing of the basic concepts andformulas of wave propagation 2006 artículo científico 0122-5383 https://www.redalyc.org/articulo.oa?id=46530203 en http://www.redalyc.org/revista.oa?id=465 CT&F Ciencia, Tecnología y Futuro application/pdf ECOPETROL S.A. CT&F Ciencia, Tecnología y Futuro (Colombia) Num.2 Vol.3
title Calculation of phase and groupangles, slowness surfaces and ray tracing in transversely isotropic media
topic Ingeniería
ray path
symmetry
isotropy
anisotropy
elasticity
url https://www.redalyc.org/articulo.oa?id=46530203