Tectónica extensional en el borde occidental de la Cuenca VascoCantábrica (Cordillera Cantábrica, NO de España)

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dc.contributor.authorEspina, R. G.
dc.date.accessioned2016-09-22T09:32:03Z
dc.date.available2016-09-22T09:32:03Z
dc.date.issued1996
dc.description.abstractA geological cross-section in the western border of the Vasco-Cantabrian Basin show extensional faults active during Permo-Mesozoic sedimentation , as well as the tectonic inversion of these faults during Alpine deformation. The hercynian basement of the Cantabrian Zone was deformed together with the Meso-Cenozoic cover during the extension and subsequent compression, without the existence of detachments betwen them. Cross-section restauration allow to reconstruct the sedimentary basins from Permian to Upper Cretaceus times. The calculated extension during this time is of about 7.5 Km and the alpine shortening of 20 Km.en_US
dc.identifier.urihttp://hdl.handle.net/10272/12674
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherBasementen_US
dc.subject.otherCoveren_US
dc.subject.otherVasco-Cantabrian Basinen_US
dc.subject.otherExtensionen_US
dc.subject.otherTectonic inversionen_US
dc.titleTectónica extensional en el borde occidental de la Cuenca VascoCantábrica (Cordillera Cantábrica, NO de España)en_US
dc.titleExtensional tectonics in the western border of the Vasco-Cantabrian Basin (Cantabrian Mountains, NW of Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-4, (1996)