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Stress fields, Alpine deformation and associated Neogene-Quaternary volcanism in the Betic foreland of the province of Ciudad Real, Central Spam

dc.contributor.authorVegas, Ramón
dc.contributor.authorRincón Calero, P. J.
dc.date.accessioned2017-02-21T13:36:19Z
dc.date.available2017-02-21T13:36:19Z
dc.date.issued1995
dc.identifier.urihttp://hdl.handle.net/10272/13360
dc.description.abstractThe analysis of brittle structures and regional physiographic features in the province of Ciudad Real (Central Spain), leads to establish a model of neotectonic deformation in relation with the foreland of the eastern Betic Cordillera. In this model, a weak compressive stress field is responsible for flexural bending of the crust and the lithosphere, and the occurrence of the Neogene-Quaternary volcanism in the Campo de Calatravaen_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.otherBrittle mesostructureen_US
dc.subject.otherFault population analysisen_US
dc.subject.otherLithospheric bendingen_US
dc.subject.otherBetic forelanden_US
dc.subject.otherCentral Spainen_US
dc.titleCampos de esfuerzos, deformación alpina y volcanismo neógeno-cuaternario asociado en el antepaís bético de la provincia de Ciudad Real (España central)en_US
dc.titleStress fields, Alpine deformation and associated Neogene-Quaternary volcanism in the Betic foreland of the province of Ciudad Real, Central Spameng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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