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Deep structure of thè Cameros basin (Iberian Chain) from gravity data

dc.contributor.authorRivero, Luis
dc.contributor.authorGuimerà, J.
dc.contributor.authorCasas Sainz, Antonio
dc.date.accessioned2017-01-26T09:58:35Z
dc.date.available2017-01-26T09:58:35Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/13196
dc.description.abstractThe Cameros basin (Iberian Chain) developed under a very subsident extensional regime during the latest Jurassic-early Cretaceous. Its fill constitutes a magasequence o f more than 5000 m of vertical thickness. That would produce a gravity low. Nevertheless, the gravity map of this area draws a gravity high in the eastern part of the basin. We propose an explanation to this contradictionen_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.otherGravity dataen_US
dc.subject.otherIberian rangeen_US
dc.subject.otherCameros basinen_US
dc.titleEstructura profunda de la cuenca de Cameros (Cordillera Ibérica) a partir de datos gravimétricosen_US
dc.titleDeep structure of thè Cameros basin (Iberian Chain) from gravity dataeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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