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First evidence of paleoearthquakes in Carboneras Fault: A Paleoseismological study in La Serrata

dc.contributor.authorMoreno, Ximena
dc.contributor.authorMasana, E.
dc.contributor.authorGràcia, E.
dc.contributor.authorPallàs, R.
dc.contributor.authorRuano, Patricia
dc.contributor.authorColl, Miquel
dc.contributor.authorStepancíková, P.
dc.contributor.authorSantanach, P.
dc.date.accessioned2014-07-11T10:22:51Z
dc.date.available2014-07-11T10:22:51Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8511
dc.description.abstractA paleoseismological analysis was performed along the La Serrata segment of the Carboneras fault (Eastern Betics) in order to establish its seismic potential. The site was selected after a general geomorphological analysis of the whole fault and af ter a near-fault study of the surface geology. Trenches across the fault exposed colluvial wedges, which evidenced sudden deformation events (paleoear thquakes). The Carboneras is, thus, a seismogenic fault. Evidence of a minimum of four events in the last 50 ka was detected suggesting a mean recurrence period of 14 ka. The geometry of the units and S-C structures observed in trenches indicate a lef t-lateral with some reverse component movement along the fault in its most recent activityen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherCarboneras Faulten_US
dc.subject.otherEastern Beticsen_US
dc.subject.otherPaleoseismologyen_US
dc.subject.otherTrenchingen_US
dc.subject.otherNeotectonicsen_US
dc.titlePrimeras evidencias de paleoterremotos en la falla de Carboneras: estudio paleosismológico en el segmento de La Serrataen_US
dc.titleFirst evidence of paleoearthquakes in Carboneras Fault: A Paleoseismological study in La Serrataeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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