Extensión versus compresión durante el Mioceno superior en la Cuenca de Lorca (Báticas orientales)

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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.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.identifier.urihttp://hdl.handle.net/10272/9048
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.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.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 34, (2003)