Neotectónica en el antepaís castellano de las cordilleras Béticas orientales

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dc.contributor.authorRincón Calero, P. J.
dc.contributor.authorVegas, Ramón
dc.date.accessioned2016-09-20T12:11:22Z
dc.date.available2016-09-20T12:11:22Z
dc.date.issued1996
dc.description.abstractThe major morphotectonic features in the foreland of the Eastern Betics can be explained within the frame of the weak compressive stress field originated in the Prebetic fold and thrust belt. This NW directed compression is partitioned by N130°-150° dextral strike-slip corridors and orthogonal crustal flexures. The Neogene-Quaternary volcanism and the distribution of seismicity can be also considered within this compressive neotectonic regimenen_US
dc.identifier.urihttp://hdl.handle.net/10272/12661
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.otherStress configurationen_US
dc.subject.otherMorphotectonicsen_US
dc.subject.otherCrustal flexuresen_US
dc.subject.otherIntraplate accommodationen_US
dc.subject.otherEastern Betics forelanden_US
dc.titleNeotectónica en el antepaís castellano de las cordilleras Béticas orientalesen_US
dc.titleNeotectonics in the Castilian foreland of the Betic cordilleraseng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-4, (1996)