Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia

The SW of Iberia is currently undergoing compression related to the convergence between Nubia and Iberia. Multiple compressive structures, and their related seismic activity, have been documented along the diffuse Nubia-Iberia plate boundary, including the Gorringe bank west of the Gulf of Cadiz, an...

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Detalhes bibliográficos
Autores: Ramos Ordoño, Adrià, Fernández, Òscar, Terrinha, P., Muñoz, J. A.
Tipo de documento: artigo
Estado:Versão publicada
Data de publicação:2017
País:España
Recursos:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Repositório:Recercat. Dipósit de la Recerca de Catalunya
OAI Identifier:oai:recercat.cat:2445/161520
Acesso em linha:https://hdl.handle.net/2445/161520
Access Level:Acceso aberto
Palavra-chave:Paleogeografia
Geofísica
Sedimentologia
Península Ibèrica
Paleogeography
Geophysics
Sedimentology
Iberian Peninsula
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spelling Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW IberiaRamos Ordoño, AdriàFernández, ÒscarTerrinha, P.Muñoz, J. A.PaleogeografiaGeofísicaSedimentologiaPenínsula IbèricaPaleogeographyGeophysicsSedimentologyIberian PeninsulaThe SW of Iberia is currently undergoing compression related to the convergence between Nubia and Iberia. Multiple compressive structures, and their related seismic activity, have been documented along the diffuse Nubia-Iberia plate boundary, including the Gorringe bank west of the Gulf of Cadiz, and the Betic-Rif orogen to the east. Despite seismic activity indicating a dominant compressive stress along the Algarve margin in the Gulf of Cadiz, the structures at the origin of this seismicity remain elusive. This paper documents the contractional structures that provide linkage across the Gulf of Cadiz and play a major role in defining the present-day seismicity and bathymetry of this area. The structures described in this paper caused the Neogene inversion of the Jurassic oblique passive margin that formed between the central Atlantic and the Ligurian Tethys. This example of a partially inverted margin provides insights into the factors that condition the inversion of passive margins.Wiley2020202020172020info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersion30 p.application/pdfapplication/pdfhttps://hdl.handle.net/2445/161520Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)reponame:Recercat. Dipósit de la Recerca de Catalunyainstname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)InglésReproducció del document publicat a: https://doi.org/10.1002/2016TC004262Tectonics, 2017, vol. 36, num. 2, p. 257-286https://doi.org/10.1002/2016TC004262(c) American Geophysical Union (AGU), 2017info:eu-repo/semantics/openAccessoai:recercat.cat:2445/1615202026-05-29T05:05:01Z
dc.title.none.fl_str_mv Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia
title Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia
spellingShingle Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia
Ramos Ordoño, Adrià
Paleogeografia
Geofísica
Sedimentologia
Península Ibèrica
Paleogeography
Geophysics
Sedimentology
Iberian Peninsula
title_short Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia
title_full Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia
title_fullStr Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia
title_full_unstemmed Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia
title_sort Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia
dc.creator.none.fl_str_mv Ramos Ordoño, Adrià
Fernández, Òscar
Terrinha, P.
Muñoz, J. A.
author Ramos Ordoño, Adrià
author_facet Ramos Ordoño, Adrià
Fernández, Òscar
Terrinha, P.
Muñoz, J. A.
author_role author
author2 Fernández, Òscar
Terrinha, P.
Muñoz, J. A.
author2_role author
author
author
dc.subject.none.fl_str_mv Paleogeografia
Geofísica
Sedimentologia
Península Ibèrica
Paleogeography
Geophysics
Sedimentology
Iberian Peninsula
topic Paleogeografia
Geofísica
Sedimentologia
Península Ibèrica
Paleogeography
Geophysics
Sedimentology
Iberian Peninsula
description The SW of Iberia is currently undergoing compression related to the convergence between Nubia and Iberia. Multiple compressive structures, and their related seismic activity, have been documented along the diffuse Nubia-Iberia plate boundary, including the Gorringe bank west of the Gulf of Cadiz, and the Betic-Rif orogen to the east. Despite seismic activity indicating a dominant compressive stress along the Algarve margin in the Gulf of Cadiz, the structures at the origin of this seismicity remain elusive. This paper documents the contractional structures that provide linkage across the Gulf of Cadiz and play a major role in defining the present-day seismicity and bathymetry of this area. The structures described in this paper caused the Neogene inversion of the Jurassic oblique passive margin that formed between the central Atlantic and the Ligurian Tethys. This example of a partially inverted margin provides insights into the factors that condition the inversion of passive margins.
publishDate 2017
dc.date.none.fl_str_mv 2017
2020
2020
2020
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/2445/161520
url https://hdl.handle.net/2445/161520
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Reproducció del document publicat a: https://doi.org/10.1002/2016TC004262
Tectonics, 2017, vol. 36, num. 2, p. 257-286
https://doi.org/10.1002/2016TC004262
dc.rights.none.fl_str_mv (c) American Geophysical Union (AGU), 2017
info:eu-repo/semantics/openAccess
rights_invalid_str_mv (c) American Geophysical Union (AGU), 2017
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 30 p.
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Wiley
publisher.none.fl_str_mv Wiley
dc.source.none.fl_str_mv Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
reponame:Recercat. Dipósit de la Recerca de Catalunya
instname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
instname_str Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
reponame_str Recercat. Dipósit de la Recerca de Catalunya
collection Recercat. Dipósit de la Recerca de Catalunya
repository.name.fl_str_mv
repository.mail.fl_str_mv
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