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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Authors: Martín Velázquez, Silvia; Elorza, F. J.
Format: Article
Publication date:2007
Country:España
Institution:Universidad de Huelva (UHU)
Repository:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Language:Spanish
OAI Identifier:oai:ariasmontano.uhu.es:10272/8401
Online Access:http://hdl.handle.net/10272/8401
Access Level:Open access
Keyword:Lithospheric deformation
Spanish Central System
Duero basin
Tajo basin
Finite element modelling
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author Martín Velázquez, Silvia
author2 Elorza, F. J.
author2_role author
author_browse Elorza, F. J.
Martín Velázquez, Silvia
author_facet Martín Velázquez, Silvia
Elorza, F. J.
author_role author
collection Arias Montano. Repositorio Institucional de la Universidad de Huelva
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
eu_rights_str_mv openAccess
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id ES_095c8f4e94e055a3a3eecaddae4b8a39
institution Universidad de Huelva (UHU)
instname_str Universidad de Huelva (UHU)
language spa
network_acronym_str ES
network_name_str España
oai_identifier_str oai:ariasmontano.uhu.es:10272/8401
publishDate 2007
publishDateSort 2007
reponame_str Arias Montano. Repositorio Institucional de la Universidad de Huelva
spelling 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 Martín Velázquez, Silvia Elorza, F. J. Lithospheric deformation Spanish Central System Duero basin Tajo basin Finite element modelling 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 http://hdl.handle.net/10272/8401
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 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_short 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
topic Lithospheric deformation
Spanish Central System
Duero basin
Tajo basin
Finite element modelling
topic_facet Lithospheric deformation
Spanish Central System
Duero basin
Tajo basin
Finite element modelling
url http://hdl.handle.net/10272/8401