Neotectónica en el antepaís castellano de las cordilleras Béticas orientales

The major morphotectonic features in the foreland of the Eastern Betics can be explained within the frame of the weak compressive stress field originated in the Prebetic fold and thrust belt. This NW directed compression is partitioned by N130°-150° dextral strike-slip corridors and orthogonal crust...

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Detalles Bibliográficos
Autores: Rincón Calero, P. J., Vegas, Ramón
Tipo de recurso: artículo
Fecha de publicación:1996
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:10272/12661
Acceso en línea:http://hdl.handle.net/10272/12661
Access Level:acceso abierto
Palabra clave:Stress configuration
Morphotectonics
Crustal flexures
Intraplate accommodation
Eastern Betics foreland
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spelling Neotectónica en el antepaís castellano de las cordilleras Béticas orientalesNeotectonics in the Castilian foreland of the Betic cordillerasRincón Calero, P. J.Vegas, RamónStress configurationMorphotectonicsCrustal flexuresIntraplate accommodationEastern Betics forelandThe major morphotectonic features in the foreland of the Eastern Betics can be explained within the frame of the weak compressive stress field originated in the Prebetic fold and thrust belt. This NW directed compression is partitioned by N130°-150° dextral strike-slip corridors and orthogonal crustal flexures. The Neogene-Quaternary volcanism and the distribution of seismicity can be also considered within this compressive neotectonic regimenSociedad Geológica de España19961996-01-0119961996-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/12661reponame: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:10272/126612026-06-02T14:58:11Z
dc.title.none.fl_str_mv Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
Neotectonics in the Castilian foreland of the Betic cordilleras
title Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
spellingShingle Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
Rincón Calero, P. J.
Stress configuration
Morphotectonics
Crustal flexures
Intraplate accommodation
Eastern Betics foreland
title_short Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
title_full Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
title_fullStr Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
title_full_unstemmed Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
title_sort Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
dc.creator.none.fl_str_mv Rincón Calero, P. J.
Vegas, Ramón
author Rincón Calero, P. J.
author_facet Rincón Calero, P. J.
Vegas, Ramón
author_role author
author2 Vegas, Ramón
author2_role author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Stress configuration
Morphotectonics
Crustal flexures
Intraplate accommodation
Eastern Betics foreland
topic Stress configuration
Morphotectonics
Crustal flexures
Intraplate accommodation
Eastern Betics foreland
description The major morphotectonic features in the foreland of the Eastern Betics can be explained within the frame of the weak compressive stress field originated in the Prebetic fold and thrust belt. This NW directed compression is partitioned by N130°-150° dextral strike-slip corridors and orthogonal crustal flexures. The Neogene-Quaternary volcanism and the distribution of seismicity can be also considered within this compressive neotectonic regimen
publishDate 1996
dc.date.none.fl_str_mv 1996
1996-01-01
1996
1996-01-01
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/10272/12661
url http://hdl.handle.net/10272/12661
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.publisher.none.fl_str_mv Sociedad Geológica de España
publisher.none.fl_str_mv Sociedad Geológica de España
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
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repository.mail.fl_str_mv
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