Geodynamic implications derived from Numidian-like distal turbidites deposited along the Internal–External Domain Boundary of the Betic Cordillera (S Spain)
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Campo DC | Valor | Idioma |
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dc.contributor | Evolución Geodinámica de la Cordillera Bética Oriental y de la Plataforma Marina de Alicante | es |
dc.contributor.author | Alcalá, Francisco J. | - |
dc.contributor.author | Guerrera, Francesco | - |
dc.contributor.author | Martín-Martín, Manuel | - |
dc.contributor.author | Raffaelli, Giuliana | - |
dc.contributor.author | Serrano Lozano, Francisco | - |
dc.contributor.other | Universidad de Alicante. Departamento de Ciencias de la Tierra y del Medio Ambiente | es |
dc.date.accessioned | 2013-03-22T11:25:42Z | - |
dc.date.available | 2013-03-22T11:25:42Z | - |
dc.date.issued | 2012-11-21 | - |
dc.identifier.citation | ALCALÁ, Francisco J., et al. “Geodynamic implications derived from Numidian-like distal turbidites deposited along the Internal–External Domain Boundary of the Betic Cordillera (S Spain)”. Terra Nova. Vol. 25, No. 2 (Apr. 2013). ISSN 0954-4879, pp. 119-129 | es |
dc.identifier.issn | 0954-4879 (Print) | - |
dc.identifier.issn | 1365-3121 (Online) | - |
dc.identifier.uri | http://hdl.handle.net/10045/27494 | - |
dc.description.abstract | New data reveal Early Burdigalian ‘Numidian-like lithofacies’ in successions of the internal (southernmost) part of the South Iberian Margin (SIM) and the south-western margin of the Mesomediterranean Microplate (MM). The well-known Numidian Formation was deposited in the external (Massylian) sub-domain of the Maghrebian Flysch Basin (a south-western branch of the Tethys Ocean). The anomalous occurrence of ‘Numidian-like lithofacies’ is induced by the particular Early Miocene palaeogeographical and geodynamic complexity of the sector. This consisted of a ‘triple point’ with a dextral transform fault between the SIM and the MM-Maghrebian Flysch Basin system. In this framework, the ageing of Iberian reliefs and the MM collapse, coupled with an African Margin upbulging, and a shortening of the Maghrebian Flysch Basin (both related to the subduction), could have resulted in the arrival of the Numidian depositional system from so far away. | es |
dc.description.sponsorship | This research was supported by Urbino University ‘Carlo Bo’ grant (responsible F. Guerrera), Spanish CICYT Research Projects CGL2009-09249, CGL2011-30153-CO2-02, and CGL2012-32169, Portuguese FCT Research Project PTDC⁄CLI⁄72585⁄2006, Research Groups and projects of the Generalitat Valenciana from Alicante University (CTMA-IGA), and Research Group 146 of the Junta de Andalucía. The first author is also grateful to the Portuguese FCT ‘Ciência 2008’ Programme Contract C2008-IST⁄CVRM.1. | es |
dc.language | eng | es |
dc.publisher | Blackwell Publishing | es |
dc.rights | The definitive version is available at http://onlinelibrary.wiley.com/ | es |
dc.subject | Numidian | es |
dc.subject | Betic Cordillera | es |
dc.subject | Geodynamic implications | es |
dc.subject.other | Geodinámica Interna | es |
dc.title | Geodynamic implications derived from Numidian-like distal turbidites deposited along the Internal–External Domain Boundary of the Betic Cordillera (S Spain) | es |
dc.type | info:eu-repo/semantics/article | es |
dc.peerreviewed | si | es |
dc.identifier.doi | 10.1111/ter.12014 | - |
dc.relation.publisherversion | http://dx.doi.org/10.1111/ter.12014 | es |
dc.rights.accessRights | info:eu-repo/semantics/restrictedAccess | es |
dc.relation.projectID | info:eu-repo/grantAgreement/MICINN//CGL2009-09249 | - |
dc.relation.projectID | info:eu-repo/grantAgreement/MICINN//CGL2011-30153-C02-02 | - |
dc.relation.projectID | info:eu-repo/grantAgreement/MINECO//CGL2012-32169 | - |
Aparece en las colecciones: | INV - GEODIN - Artículos de Revistas |
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2012_Numidian_like_OMNF_TER.pdf | Versión final (acceso restringido) | 3,28 MB | Adobe PDF | Abrir Solicitar una copia |
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