Sismicidad en el antepaís de las cordilleras Béticas orientales: determinación del tensor de esfuerzos actual

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dc.contributor.authorRincón Calero, P. J.
dc.contributor.authorGiner Robles, J. L.
dc.contributor.authorVegas, Ramón
dc.contributor.authorVicente, Gerardo de
dc.date.accessioned2016-09-21T11:47:34Z
dc.date.available2016-09-21T11:47:34Z
dc.date.issued1996
dc.description.abstractThe seismicity in the Castilian foreland of the Betic Cordilleras is in accordance with an intraplate compressive stress-field that is characterized by the coexistence of two stress tensors: SHmax N140°-160°E (regional tensor) and SHmax N60°-70°E (secondary tensor). The subsequent intraplate deformation is accommodated by means of dextral strike-slip faults and crustal flexures. The seismic activity seems to be concentrated in some N130°-150°E fault zones in the front of the Alcaraz Arcen_US
dc.identifier.urihttp://hdl.handle.net/10272/12669
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 tensoren_US
dc.subject.otherFault plane mechanismsen_US
dc.subject.otherFault population analysisen_US
dc.subject.otherBetic forelanden_US
dc.subject.otherSeismicityen_US
dc.titleSismicidad en el antepaís de las cordilleras Béticas orientales: determinación del tensor de esfuerzos actualen_US
dc.titleSeismicity in the castillan forelandl of de betic cordilleras: neotectonic stress tensor determinationeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-4, (1996)