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Extension versus contraction during the Upper Miocene in the Lorca basin (eastern Betics)

dc.contributor.authorBooth Rea, G.
dc.contributor.authorAzañón, José Miguel
dc.date.accessioned2014-10-31T09:52:15Z
dc.date.available2014-10-31T09:52:15Z
dc.date.issued2003
dc.identifier.urihttp://hdl.handle.net/10272/9048
dc.description.abstractStructural and paleostress analysis of the Tortonian sedimentary cover of the Lorca basin (eastern Betics), shows the existence of alternating extensional and convergent tectonics during this period. With ENE/ WSW-oriented Tortonian folds being cut and tilted by upper Tortonian normal faults with NW/SE to SW/ NE tectonic transport, which define a paleostress tensor indicative of radial-extension. These faults were later folded during further uppermost-Tortonian to Messinian convergenceen_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.otherExtensiónen_US
dc.subject.otherConvergenceen_US
dc.subject.otherTortonianen_US
dc.subject.otherLorca basinen_US
dc.subject.otherEastern Beticsen_US
dc.titleExtensión versus compresión durante el Mioceno superior en la Cuenca de Lorca (Báticas orientales)en_US
dc.titleExtension versus contraction during the Upper Miocene in the Lorca basin (eastern Betics)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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