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Structural and geometric features of the Lorca-Alhama strike-slip fault

dc.contributor.authorSilva, P. G.
dc.contributor.authorGoy, José L.
dc.contributor.authorZazo, C.
dc.date.accessioned2019-05-29T10:12:59Z
dc.date.available2019-05-29T10:12:59Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/10272/16323
dc.description.abstractThe Lorca-Alhama fault is one of the more tectonic and seismically active sinistraI strike-slip fault of the eastern Betics. Its complex structural pattern records simultaneous development of ex- tensional and contractional features, which can be explained by a simple sinistral shear model. Spatial coincidence of structural and geometric diagnostic features of segment boundaries along the strike of the fault, are reflecting the segmented nature of this tectonic accidentes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherStructural patternes_ES
dc.subject.otherGeometryes_ES
dc.subject.otherSimple sheares_ES
dc.subject.otherFault segmentationes_ES
dc.subject.otherLorca-Alhama faultes_ES
dc.subject.otherEastern Beticses_ES
dc.titleCaracterísticas estructurales y geométricas de la falla de desgarre de Lorca-Alhamaes_ES
dc.titleStructural and geometric features of the Lorca-Alhama strike-slip faulteng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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