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dc.contributor.authorMasana, E.-
dc.contributor.authorPallàs, R.-
dc.contributor.authorOrtuño, María-
dc.contributor.authorLópez, R.-
dc.contributor.authorGómez-Novell-
dc.contributor.authorBordonau, Jaume-
dc.contributor.authorKhazaradze, G.-
dc.contributor.authorBaguer, A.-
dc.contributor.authorMoreno, Ximena-
dc.contributor.authorGràcia, Eulàlia-
dc.date.accessioned2018-10-30T13:05:37Z-
dc.date.available2018-10-30T13:05:37Z-
dc.date.issued2018-06-
dc.identifierisbn: 978-84-09-02473-5-
dc.identifier.citationIberfault 2018 : Avances en el estudio de Fallas Activas, Terremotos y Peligrosidad Sísmica de Iberia : III Reunión Ibérica sobre Fallas Activas y Paleosismología : Volumen de resúmenes: 83-86 (2018)-
dc.identifier.urihttp://hdl.handle.net/10261/171746-
dc.descriptionInciativa Ibérica para el Estudio de las Fallas Activas, Tercera Reunión Ibérica sobre Fallas Activas y Paleosismología IBERFAULT 2018 - Third Iberian Meeting on Active Faults and Paleoseismology, 11-13 June 2018, Alicante, Spain.-- 4 pages, 2 figures-
dc.description.abstractThe Carboneras fault, the southernmost fault of the Eastern Betic Shear Zone, cannot be associated to significative historical or instrumental seismicity in spite of showing surface expression of being an active left lateral fault. Revision of the paleoseismic data at Los Trances and El Hacho sites, on the northwestern edge of La Serrata range, provides the first evidence of this fault being seismogenic. The fault has undergone a minimum of 5 paleoearthquakes since 133-56.6 ka which can be observed in the geological record at both sites (only the youngest is uniquely detected at El Hacho). This is a minimum amount of earthquakes given the non-continuous sedimentation sequence recorded in the area. A maximum recurrence period of 26-11 ka is obtained since 133-56.6 ka. However, when only the last 3 events are considered, the recurrence lowers down (13-9 ka) suggesting: or 1) clustering in the most recent period, or, again, 2) incompleteness of the seismic history owing to a discontinuous geological record. The 3D analysis at El Hacho provides also evidence for the lateral slip per event, which might be of 1.5m, corresponding to a Mw 6.9-7 earthquake-
dc.rightsopenAccess-
dc.subjectSeismic history-
dc.subjectSeismic parameters-
dc.subjectTrenching-
dc.subjectCarboneras fault-
dc.titleThe Carboneras fault (revisited) as a seismic source-
dc.title.alternativePrimeros datos paleosísmicos en la falla de Carboneras: reinterpretación-
dc.typecomunicación de congreso-
dc.relation.publisherversionhttp://home.iberfault.org/-
dc.date.updated2018-10-30T13:05:37Z-
dc.description.versionPeer Reviewed-
dc.language.rfc3066eng-
dc.relation.csic-
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