Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional
A combined structural and AMS analysis is made in Upper Cretaceous rocks from the periclinal closure of the Biscay Synclinorium (Basque-Cantabrian basin). Fieldwork has led to the recognition of a broad band with a pervasive foliation along the NE limb. The magnetic fabrics are grouped into two zone...
| Autores: | , , , , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2017 |
| 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:10272/15139 |
| Acceso en línea: | http://hdl.handle.net/10272/15139 |
| Access Level: | acceso abierto |
| Palabra clave: | Fábrica magnética Sinclinorio de Bizkaia Cuenca Vasco-Cantábrica Zona de cizalla Magnetic fabrics Biscay Synclinorium Basque-Cantabrian basin Shear zone |
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Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regionalMagnetic fabric analysis of the Biscay Synclinorium: Implications for the regional tectonicsVegas, NéstorAranguren, A.Rodríguez, LidiaCuevas, JuliaTubía, José MaríaEsteban, José JuliánFábrica magnéticaSinclinorio de BizkaiaCuenca Vasco-CantábricaZona de cizallaMagnetic fabricsBiscay SynclinoriumBasque-Cantabrian basinShear zoneA combined structural and AMS analysis is made in Upper Cretaceous rocks from the periclinal closure of the Biscay Synclinorium (Basque-Cantabrian basin). Fieldwork has led to the recognition of a broad band with a pervasive foliation along the NE limb. The magnetic fabrics are grouped into two zones: 1) the samples from the core record magnetic lineations coincident with the SO/S 1 intersection lineation that are parallel to the synclinorium axis, and 2) the magnetic lineations from the NE limb are orthogonal to the synclinorium axis and concentrate around the down-dip direction of S 1. This partitioning of magnetic fabrics suggests in creasing deformation from the core, characterised by mixed (sedimentary and tectonic) magnetic fabrics, to the northeastern limb, where tectonic fabrics prevail. Field data and magnetic fabrics are consistent with an unusually high deformation in the NE limb of the synclinorium, which could be associated with a hitherto unknown shear zone at regional scale. A top to the NE movement of the shear zone would explain the trend of the magnetic lineation in the northeastern limb of the Biscay SynclinoriumSociedad Geológica de España20172017-01-0120172017-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/15139reponame: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:10272/151392026-06-02T14:58:11Z |
| dc.title.none.fl_str_mv |
Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional Magnetic fabric analysis of the Biscay Synclinorium: Implications for the regional tectonics |
| title |
Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional |
| spellingShingle |
Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional Vegas, Néstor Fábrica magnética Sinclinorio de Bizkaia Cuenca Vasco-Cantábrica Zona de cizalla Magnetic fabrics Biscay Synclinorium Basque-Cantabrian basin Shear zone |
| title_short |
Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional |
| title_full |
Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional |
| title_fullStr |
Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional |
| title_full_unstemmed |
Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional |
| title_sort |
Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional |
| dc.creator.none.fl_str_mv |
Vegas, Néstor Aranguren, A. Rodríguez, Lidia Cuevas, Julia Tubía, José María Esteban, José Julián |
| author |
Vegas, Néstor |
| author_facet |
Vegas, Néstor Aranguren, A. Rodríguez, Lidia Cuevas, Julia Tubía, José María Esteban, José Julián |
| author_role |
author |
| author2 |
Aranguren, A. Rodríguez, Lidia Cuevas, Julia Tubía, José María Esteban, José Julián |
| author2_role |
author author author author author |
| dc.contributor.none.fl_str_mv |
|
| dc.subject.none.fl_str_mv |
Fábrica magnética Sinclinorio de Bizkaia Cuenca Vasco-Cantábrica Zona de cizalla Magnetic fabrics Biscay Synclinorium Basque-Cantabrian basin Shear zone |
| topic |
Fábrica magnética Sinclinorio de Bizkaia Cuenca Vasco-Cantábrica Zona de cizalla Magnetic fabrics Biscay Synclinorium Basque-Cantabrian basin Shear zone |
| description |
A combined structural and AMS analysis is made in Upper Cretaceous rocks from the periclinal closure of the Biscay Synclinorium (Basque-Cantabrian basin). Fieldwork has led to the recognition of a broad band with a pervasive foliation along the NE limb. The magnetic fabrics are grouped into two zones: 1) the samples from the core record magnetic lineations coincident with the SO/S 1 intersection lineation that are parallel to the synclinorium axis, and 2) the magnetic lineations from the NE limb are orthogonal to the synclinorium axis and concentrate around the down-dip direction of S 1. This partitioning of magnetic fabrics suggests in creasing deformation from the core, characterised by mixed (sedimentary and tectonic) magnetic fabrics, to the northeastern limb, where tectonic fabrics prevail. Field data and magnetic fabrics are consistent with an unusually high deformation in the NE limb of the synclinorium, which could be associated with a hitherto unknown shear zone at regional scale. A top to the NE movement of the shear zone would explain the trend of the magnetic lineation in the northeastern limb of the Biscay Synclinorium |
| publishDate |
2017 |
| dc.date.none.fl_str_mv |
2017 2017-01-01 2017 2017-01-01 |
| 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/10272/15139 |
| url |
http://hdl.handle.net/10272/15139 |
| 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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1869425214249500672 |
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15,81155 |