Alpine tectonic framework of south-western Duero basin

The tectonic activity in the south-western area of the Spanish Northern Meseta (Ciudad Rodrigo and Duero basins) during most of the Tertiary was determined by u transpressive regime that reactivated Hercynian to Late-Hercynian faults. The record of the Alpine Orogeny is complex because the sedimenta...

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Detalhes bibliográficos
Autores: Santisteban Navarro, Juan Ignacio, Mediavilla López, Rosa María, Martín Serrano, Ángel
Tipo de documento: capítulo de livro
Data de publicação:1996
País:España
Recursos:Universidad Complutense de Madrid (UCM)
Repositório:Docta Complutense
Idioma:inglês
OAI Identifier:oai:docta.ucm.es:20.500.14352/60509
Acesso em linha:https://hdl.handle.net/20.500.14352/60509
Access Level:Acceso aberto
Palavra-chave:551.3.051(460)
551.24(460)
Alpine tectonics
Spanish
Duero Basins
Iberian Peninsula
Geología estratigráfica
2506.19 Estratigrafía
id ES_1fbb1d8b940d869ea1908769d928b2c9
oai_identifier_str oai:docta.ucm.es:20.500.14352/60509
network_acronym_str ES
network_name_str España
repository_id_str
spelling Alpine tectonic framework of south-western Duero basinSantisteban Navarro, Juan IgnacioMediavilla López, Rosa MaríaMartín Serrano, Ángel551.3.051(460)551.24(460)Alpine tectonicsSpanishDuero BasinsIberian PeninsulaGeología estratigráfica2506.19 EstratigrafíaThe tectonic activity in the south-western area of the Spanish Northern Meseta (Ciudad Rodrigo and Duero basins) during most of the Tertiary was determined by u transpressive regime that reactivated Hercynian to Late-Hercynian faults. The record of the Alpine Orogeny is complex because the sedimentary record indicates a compresive regime in the sour e areas coeval with the extensionall to transpresive regime indicated by normal or strike-slip faults. This duality is due 10 the geotectonics position of this area between two compressive areas, the Cantabrian Range and the Central System, and the extensional Atlantic margin.Cambridge University PressFriend, Peter F.Dabrio, Cristino J.Universidad Complutense de Madrid19961996-01-0119961996-01-01book parthttp://purl.org/coar/resource_type/c_3248info:eu-repo/semantics/bookPartapplication/pdfhttps://hdl.handle.net/20.500.14352/60509reponame:Docta Complutenseinstname:Universidad Complutense de Madrid (UCM)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessoai:docta.ucm.es:20.500.14352/605092026-06-02T12:44:21Z
dc.title.none.fl_str_mv Alpine tectonic framework of south-western Duero basin
title Alpine tectonic framework of south-western Duero basin
spellingShingle Alpine tectonic framework of south-western Duero basin
Santisteban Navarro, Juan Ignacio
551.3.051(460)
551.24(460)
Alpine tectonics
Spanish
Duero Basins
Iberian Peninsula
Geología estratigráfica
2506.19 Estratigrafía
title_short Alpine tectonic framework of south-western Duero basin
title_full Alpine tectonic framework of south-western Duero basin
title_fullStr Alpine tectonic framework of south-western Duero basin
title_full_unstemmed Alpine tectonic framework of south-western Duero basin
title_sort Alpine tectonic framework of south-western Duero basin
dc.creator.none.fl_str_mv Santisteban Navarro, Juan Ignacio
Mediavilla López, Rosa María
Martín Serrano, Ángel
author Santisteban Navarro, Juan Ignacio
author_facet Santisteban Navarro, Juan Ignacio
Mediavilla López, Rosa María
Martín Serrano, Ángel
author_role author
author2 Mediavilla López, Rosa María
Martín Serrano, Ángel
author2_role author
author
dc.contributor.none.fl_str_mv Friend, Peter F.
Dabrio, Cristino J.
Universidad Complutense de Madrid
dc.subject.none.fl_str_mv 551.3.051(460)
551.24(460)
Alpine tectonics
Spanish
Duero Basins
Iberian Peninsula
Geología estratigráfica
2506.19 Estratigrafía
topic 551.3.051(460)
551.24(460)
Alpine tectonics
Spanish
Duero Basins
Iberian Peninsula
Geología estratigráfica
2506.19 Estratigrafía
description The tectonic activity in the south-western area of the Spanish Northern Meseta (Ciudad Rodrigo and Duero basins) during most of the Tertiary was determined by u transpressive regime that reactivated Hercynian to Late-Hercynian faults. The record of the Alpine Orogeny is complex because the sedimentary record indicates a compresive regime in the sour e areas coeval with the extensionall to transpresive regime indicated by normal or strike-slip faults. This duality is due 10 the geotectonics position of this area between two compressive areas, the Cantabrian Range and the Central System, and the extensional Atlantic margin.
publishDate 1996
dc.date.none.fl_str_mv 1996
1996-01-01
1996
1996-01-01
dc.type.none.fl_str_mv book part
http://purl.org/coar/resource_type/c_3248
dc.type.openaire.fl_str_mv info:eu-repo/semantics/bookPart
format bookPart
dc.identifier.none.fl_str_mv https://hdl.handle.net/20.500.14352/60509
url https://hdl.handle.net/20.500.14352/60509
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
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
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Cambridge University Press
publisher.none.fl_str_mv Cambridge University Press
dc.source.none.fl_str_mv reponame:Docta Complutense
instname:Universidad Complutense de Madrid (UCM)
instname_str Universidad Complutense de Madrid (UCM)
reponame_str Docta Complutense
collection Docta Complutense
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1869404417624637441
score 15.300719

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