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Refining seismic parameters in low seismicity areas by 3D trenching: TheAlhama de Murcia fault, SE Iberia

dc.contributor.authorFerrater, Marta
dc.contributor.authorOrtuño, María
dc.contributor.authorMasana, Eulàlia
dc.contributor.authorPallàs, Raimon
dc.contributor.authorPerea Manera, Héctor
dc.contributor.authorBaize, Stephane
dc.contributor.authorMartínez Díaz, José Jesús
dc.contributor.authorGarcía Meléndez, Eduardo
dc.contributor.authorEcheverria, Anna
dc.contributor.authorRockwell, Thomas K.
dc.contributor.authorSharp, Warren D.
dc.contributor.authorMedialdea, Alicia
dc.contributor.authorRhodes, Edward J.
dc.date.accessioned2023-06-18T05:59:02Z
dc.date.available2023-06-18T05:59:02Z
dc.date.issued2016-06
dc.description.abstracthree-dimensional paleoseismology in strike-slip faults with slip rates less than 1 mm per year involves a greatmethodological challenge. We adapted 3D trenching to track buried channels offset by the Alhama de Murciaseismogenic left-lateral strike-slip fault (SE Iberia). A fault net slip of 0.9 ± 0.1 mm/yr was determined usingstatistical analysis of piercing lines for one buried channel, whose age is constrained between 15.2 ± 1.1 kaand 21.9–22.3 cal BP. This value is larger and more accurate than the previously published slip rates for thisfault. The minimum number offive paleo-earthquakes identified since the deposition of dated layers suggestsa maximum average recurrence interval of approximately 5 ka. The combination of both seismic parametersyields a maximum slip per event between 5.3 and 6.3 m. We show that accurately planned trenching strategiesand data processing may be key to obtaining robust paleoseismic parameters in low seismicity ares
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Ciencia e Innovación
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/58875
dc.identifier.doi10.1016/j.tecto.2016.05.020
dc.identifier.issn0040-1951
dc.identifier.officialurlhttps://www.sciencedirect.com/journal/tectonophysics/vol/680/suppl/C
dc.identifier.relatedurlhttp://www.elsevier.com/locate/tecto
dc.identifier.urihttps://hdl.handle.net/20.500.14352/23697
dc.journal.titleTectonophysics
dc.language.isoeng
dc.page.final128
dc.page.initial122
dc.publisherElsevier
dc.relation.projectIDSHAKE CGL2011-30005-C02-02
dc.relation.projectIDRISKNAT-2014SGR/1243
dc.rights.accessRightsrestricted access
dc.subject.cdu551.2/.3
dc.subject.cdu550.34
dc.subject.keywordPaleoseismology
dc.subject.keywordStrike-slip fault
dc.subject.keywordRecurrence
dc.subject.keywordSlip rate Slip per event
dc.subject.keywordSE Iberian Peninsula
dc.subject.ucmGeodinámica
dc.subject.ucmSismología (Geología)
dc.subject.unesco2507 Geofísica
dc.subject.unesco2507.05 Sismología y Prospección Sísmica
dc.titleRefining seismic parameters in low seismicity areas by 3D trenching: TheAlhama de Murcia fault, SE Iberia
dc.typejournal article
dc.volume.number680
dspace.entity.typePublication
relation.isAuthorOfPublication7f2238bf-4ce8-46df-a7f1-edff1e8e34fa
relation.isAuthorOfPublicationb3891000-7686-4168-b5d2-f4822f6d2337
relation.isAuthorOfPublication.latestForDiscoveryb3891000-7686-4168-b5d2-f4822f6d2337

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