Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo

The Cenozoic deformation of the Iberian lithosphere along a NW-SE profile from the northern Duero Basin to the southern Tajo Basin, crossing Spanish Central System, has been analysed by means of a numerical simulation based in the finite element method. Lateral and vertical rheological heterogeneiti...

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Detalles Bibliográficos
Autores: Martín Velázquez, Silvia, Elorza, F. J.
Tipo de recurso: artículo
Fecha de publicación:2007
País:España
Institución:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/8401
Acceso en línea:http://hdl.handle.net/10272/8401
Access Level:acceso abierto
Palabra clave:Lithospheric deformation
Spanish Central System
Duero basin
Tajo basin
Finite element modelling
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spelling Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y TajoCenozoic deformation of the Iberian lithosphere: Spanish Central System and Duero and Tajo BasinsMartín Velázquez, SilviaElorza, F. J.Lithospheric deformationSpanish Central SystemDuero basinTajo basinFinite element modellingThe Cenozoic deformation of the Iberian lithosphere along a NW-SE profile from the northern Duero Basin to the southern Tajo Basin, crossing Spanish Central System, has been analysed by means of a numerical simulation based in the finite element method. Lateral and vertical rheological heterogeneities, Tertiary sedimentary overburden and the Alpine compressional tectonic stresses have been considered. Numerical results support a mechanism of lithospheric folding for the development of the chain and basins and a thicker lower crust below the central part of Iberia20072007-01-0120072007-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/8401reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Españolspaopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/84012026-06-02T14:58:11Z
dc.title.none.fl_str_mv Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo
Cenozoic deformation of the Iberian lithosphere: Spanish Central System and Duero and Tajo Basins
title Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo
spellingShingle Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo
Martín Velázquez, Silvia
Lithospheric deformation
Spanish Central System
Duero basin
Tajo basin
Finite element modelling
title_short Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo
title_full Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo
title_fullStr Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo
title_full_unstemmed Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo
title_sort Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo
dc.creator.none.fl_str_mv Martín Velázquez, Silvia
Elorza, F. J.
author Martín Velázquez, Silvia
author_facet Martín Velázquez, Silvia
Elorza, F. J.
author_role author
author2 Elorza, F. J.
author2_role author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Lithospheric deformation
Spanish Central System
Duero basin
Tajo basin
Finite element modelling
topic Lithospheric deformation
Spanish Central System
Duero basin
Tajo basin
Finite element modelling
description The Cenozoic deformation of the Iberian lithosphere along a NW-SE profile from the northern Duero Basin to the southern Tajo Basin, crossing Spanish Central System, has been analysed by means of a numerical simulation based in the finite element method. Lateral and vertical rheological heterogeneities, Tertiary sedimentary overburden and the Alpine compressional tectonic stresses have been considered. Numerical results support a mechanism of lithospheric folding for the development of the chain and basins and a thicker lower crust below the central part of Iberia
publishDate 2007
dc.date.none.fl_str_mv 2007
2007-01-01
2007
2007-01-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10272/8401
url http://hdl.handle.net/10272/8401
dc.language.none.fl_str_mv Español
spa
language_invalid_str_mv Español
language spa
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.source.none.fl_str_mv reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname:Universidad de Huelva (UHU)
instname_str Universidad de Huelva (UHU)
reponame_str Arias Montano. Repositorio Institucional de la Universidad de Huelva
collection Arias Montano. Repositorio Institucional de la Universidad de Huelva
repository.name.fl_str_mv
repository.mail.fl_str_mv
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