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dc.rights.licenseopenen_US
hal.structure.identifierLaboratoire de géologie de l'ENS [LGENS]
hal.structure.identifierLamont-Doherty Earth Observatory [LDEO]
dc.contributor.authorDRAB, Laureen
hal.structure.identifierGéomorphologie et géologie du Quaternaire
dc.contributor.authorHUBERT-FERRARI, Aurélia
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARTINEZ, Philippe
IDREF: 154067628
hal.structure.identifierInstitut de Physique du Globe de Paris [IPGP]
dc.contributor.authorCARLUT, Julie
hal.structure.identifierArgiles, Géochimie et Environnements sédimentaires [AGEs]
dc.contributor.authorEL OUAHABI, Meriam
dc.date.accessioned2024-05-15T08:19:18Z
dc.date.available2024-05-15T08:19:18Z
dc.date.issued2015-04
dc.identifier.issn0037-1106en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199851
dc.description.abstractEnThe North Anatolian fault (NAF) in the Marmara Sea is a significant hazard for the city of Istanbul. The use of paleoseismological data to provide an accurate seismic risk assessment for the area is constrained by the fact that the NAF system is submarine; thus a history of paleoearthquakes can be inferred only by using marine sediment cores. Here, a record of turbidites was obtained in two cores and used to reconstruct the earthquake history along the Çınarcık segment, a main branch of the NAF. Klg04 was collected from a berm north of the fault, and Klg03 was positioned in the Çınarcık basin, south of the fault. The cores were correlated using long-term geo-chemical variations in the sediment, and turbidites deposited simultaneously at both sites were then identified. Radionuclide measurements suggest the most recent turbi-dite was triggered by the 1894 C.E. M w 7.3 earthquake. We conclude that the turbidites identified at both sites are earthquake generated, based on their particular sedimento-logical and geochemical signatures; the correlation of turbidites at berm and basin sites; and the match of the most recent turbidite with a nineteenth century historical earthquake. To date older turbidites, we used carbon-14 and paleomagnetic data to build an OxCal model with a local reservoir correction of 400 50 yr. The Çınarcık segment is found to have ruptured in 1509 C.E., sometime in the fourteenth century, in 989 C.E., and in 740 C.E., with a mean recurrence interval in the range of 256–321 years. Finally, we used the earthquake record obtained to review the rupture history of the adjacent segments over the past 1500 years.
dc.language.isoENen_US
dc.title.enSubmarine Earthquake History of the Çınarcık Segment of the North Anatolian Fault in the Marmara Sea, Turkey
dc.typeArticle de revueen_US
dc.identifier.doi10.1785/0120130083en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Géophysique [physics.geo-ph]en_US
bordeaux.journalBulletin of the Seismological Society of Americaen_US
bordeaux.page622-645en_US
bordeaux.volume105en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue2Aen_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamSEDIMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierinsu-01571132
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Bulletin%20of%20the%20Seismological%20Society%20of%20America&rft.date=2015-04&rft.volume=105&rft.issue=2A&rft.spage=622-645&rft.epage=622-645&rft.eissn=0037-1106&rft.issn=0037-1106&rft.au=DRAB,%20Laureen&HUBERT-FERRARI,%20Aur%C3%A9lia&SCHMIDT,%20Sabine&MARTINEZ,%20Philippe&CARLUT,%20Julie&rft.genre=article


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