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Inversion tectonics in the central part of the Basque Arc (Basque-Cantabrian basin)

dc.contributor.authorCuevas, Julia
dc.contributor.authorAranguren, A.
dc.contributor.authorBadillo, J. M.
dc.contributor.authorTubía, José María
dc.date.accessioned2015-04-14T09:27:23Z
dc.date.available2015-04-14T09:27:23Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10333
dc.description.abstractWe report the existence of a thrust system in the central part of the Basque Arc (Basque-Cantabrian basin, Guipúzcoa). From bottom to top, the thrust system is formed by theAia, Pagoeta and Azpeitia allochthonous sheets. The kinematic and structural analysis provides a top to the NE movement, and reveals the widespread reactivation of normal faults during the Pyrenean inversion tectonicsen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherThrust systemen_US
dc.subject.otherInversion tectonicsen_US
dc.subject.otherBasque Cantabrian basinen_US
dc.titleTectónica de inversion en el sector central del Arco Vasco (Cuenca Vasco-Cantábrica)en_US
dc.titleInversion tectonics in the central part of the Basque Arc (Basque-Cantabrian basin)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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