Numerical test of the Schoemberg-Muir theory

Autores
Carcione, José M.; Picotti, Stefano; Cavallini, Fabio; Santos, Juan Enrique
Año de publicación
2012
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The Schoenberg-Muir theory states that an equivalent, homogeneous and anisotropic medium can be constructed from a layered medium composed of several thin layers, each anisotropic, under the assumption of stationarity. To test the theory we considered single transversely isotropic layers with different orientations of the symmetry axis and performed numerical simulations of wave propagation with a full-wave solver. The equivalent media have orthorhombic and monoclinic symmetries, respectively. The theory performed very well from the kinematical and dynamical points of view, even for strong anisotropy and layers described by media whose symmetry axes have different orientations.
Fil: Carcione, José M.. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia
Fil: Picotti, Stefano. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia
Fil: Cavallini, Fabio. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia
Fil: Santos, Juan Enrique. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto del Gas y del Petróleo; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
ANISOTROPY
COMPRESSIONAL WAVE (P-WAVE)
ROCK PHYSICS
SHEAR WAVE (S-WAVE)
WAVE PROPAGATION
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/195939
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/195939
network_acronym_str CONICETDig
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network_name_str CONICET Digital (CONICET)
spelling Numerical test of the Schoemberg-Muir theoryCarcione, José M.Picotti, StefanoCavallini, FabioSantos, Juan EnriqueANISOTROPYCOMPRESSIONAL WAVE (P-WAVE)ROCK PHYSICSSHEAR WAVE (S-WAVE)WAVE PROPAGATIONhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Schoenberg-Muir theory states that an equivalent, homogeneous and anisotropic medium can be constructed from a layered medium composed of several thin layers, each anisotropic, under the assumption of stationarity. To test the theory we considered single transversely isotropic layers with different orientations of the symmetry axis and performed numerical simulations of wave propagation with a full-wave solver. The equivalent media have orthorhombic and monoclinic symmetries, respectively. The theory performed very well from the kinematical and dynamical points of view, even for strong anisotropy and layers described by media whose symmetry axes have different orientations.Fil: Carcione, José M.. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; ItaliaFil: Picotti, Stefano. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; ItaliaFil: Cavallini, Fabio. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; ItaliaFil: Santos, Juan Enrique. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto del Gas y del Petróleo; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaSociety of Exploration Geophysicists2012-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/195939Carcione, José M.; Picotti, Stefano; Cavallini, Fabio; Santos, Juan Enrique; Numerical test of the Schoemberg-Muir theory; Society of Exploration Geophysicists; Geophysics; 77; 2; 6-2012; 1-90016-8033CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://mr.crossref.org/iPage?doi=10.1190%2Fgeo2011-0228.1info:eu-repo/semantics/altIdentifier/doi/10.1190/geo2011-0228.1info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:49:18Zoai:ri.conicet.gov.ar:11336/195939instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:49:19.122CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Numerical test of the Schoemberg-Muir theory
title Numerical test of the Schoemberg-Muir theory
spellingShingle Numerical test of the Schoemberg-Muir theory
Carcione, José M.
ANISOTROPY
COMPRESSIONAL WAVE (P-WAVE)
ROCK PHYSICS
SHEAR WAVE (S-WAVE)
WAVE PROPAGATION
title_short Numerical test of the Schoemberg-Muir theory
title_full Numerical test of the Schoemberg-Muir theory
title_fullStr Numerical test of the Schoemberg-Muir theory
title_full_unstemmed Numerical test of the Schoemberg-Muir theory
title_sort Numerical test of the Schoemberg-Muir theory
dc.creator.none.fl_str_mv Carcione, José M.
Picotti, Stefano
Cavallini, Fabio
Santos, Juan Enrique
author Carcione, José M.
author_facet Carcione, José M.
Picotti, Stefano
Cavallini, Fabio
Santos, Juan Enrique
author_role author
author2 Picotti, Stefano
Cavallini, Fabio
Santos, Juan Enrique
author2_role author
author
author
dc.subject.none.fl_str_mv ANISOTROPY
COMPRESSIONAL WAVE (P-WAVE)
ROCK PHYSICS
SHEAR WAVE (S-WAVE)
WAVE PROPAGATION
topic ANISOTROPY
COMPRESSIONAL WAVE (P-WAVE)
ROCK PHYSICS
SHEAR WAVE (S-WAVE)
WAVE PROPAGATION
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The Schoenberg-Muir theory states that an equivalent, homogeneous and anisotropic medium can be constructed from a layered medium composed of several thin layers, each anisotropic, under the assumption of stationarity. To test the theory we considered single transversely isotropic layers with different orientations of the symmetry axis and performed numerical simulations of wave propagation with a full-wave solver. The equivalent media have orthorhombic and monoclinic symmetries, respectively. The theory performed very well from the kinematical and dynamical points of view, even for strong anisotropy and layers described by media whose symmetry axes have different orientations.
Fil: Carcione, José M.. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia
Fil: Picotti, Stefano. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia
Fil: Cavallini, Fabio. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia
Fil: Santos, Juan Enrique. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto del Gas y del Petróleo; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description The Schoenberg-Muir theory states that an equivalent, homogeneous and anisotropic medium can be constructed from a layered medium composed of several thin layers, each anisotropic, under the assumption of stationarity. To test the theory we considered single transversely isotropic layers with different orientations of the symmetry axis and performed numerical simulations of wave propagation with a full-wave solver. The equivalent media have orthorhombic and monoclinic symmetries, respectively. The theory performed very well from the kinematical and dynamical points of view, even for strong anisotropy and layers described by media whose symmetry axes have different orientations.
publishDate 2012
dc.date.none.fl_str_mv 2012-06
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/195939
Carcione, José M.; Picotti, Stefano; Cavallini, Fabio; Santos, Juan Enrique; Numerical test of the Schoemberg-Muir theory; Society of Exploration Geophysicists; Geophysics; 77; 2; 6-2012; 1-9
0016-8033
CONICET Digital
CONICET
url http://hdl.handle.net/11336/195939
identifier_str_mv Carcione, José M.; Picotti, Stefano; Cavallini, Fabio; Santos, Juan Enrique; Numerical test of the Schoemberg-Muir theory; Society of Exploration Geophysicists; Geophysics; 77; 2; 6-2012; 1-9
0016-8033
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://mr.crossref.org/iPage?doi=10.1190%2Fgeo2011-0228.1
info:eu-repo/semantics/altIdentifier/doi/10.1190/geo2011-0228.1
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Society of Exploration Geophysicists
publisher.none.fl_str_mv Society of Exploration Geophysicists
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432

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