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dc.rights.licenseopenen_US
dc.contributor.authorGARRETT, Edd
dc.contributor.authorFUJIMURA, Osamu
dc.contributor.authorRIEDESEL, Svenja
dc.contributor.authorWALSTRA, Jan
dc.contributor.authorDEFORCE, Koen
dc.contributor.authorYOKOYAMA, Yusuke
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
dc.contributor.authorBRÜCKNER, Helmut
dc.contributor.authorDE BATIST, Marc
dc.contributor.authorHEYVAERT, Vanessa M.A.
dc.contributor.authorTEAM, Quakerecnankai
dc.date.accessioned2024-05-24T13:12:09Z
dc.date.available2024-05-24T13:12:09Z
dc.date.issued2018-06-01
dc.identifier.issn0959-6836en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200024
dc.description.abstractEnGeological investigations of coastal sediment sequences play a key role in verifying earthquake and tsunami characteristics inferred from historical records. In this paper, we present a multi-proxy investigation of a coastal lowland site facing the Nankai-Suruga megathrust and appraise evidence for tsunamis and earthquake-triggered terrestrial mass movements occurring over the last 800 years. Combining a high-resolution chronology with X-ray computed tomography and analyses of particle size, diatoms, pollen, non-pollen palynomorphs and aerial photographs, we present the most compelling geological evidence of the 1361 CE Kōan (also known as Shōhei) tsunami reported to date from any site along the megathrust. This finding is consistent with either of two recent hypotheses: a single larger rupture of both the Nankai and Tōnankai regions or two smaller ruptures separated by a few days. Enhancing the site chronology using Bayesian age modelling, we verify evidence for inundation during the 1498 CE Meiō tsunami. While previous investigations identified evidence for historically recorded tsunamis in 1605, 1707 and 1854 CE and a storm surge in 1680 or 1699 CE, we encountered a thick sand layer rather than discrete extreme wave deposits in this interval. The overprinting of evidence highlights the potential for geological records to underestimate the frequency of these events. A terrestrial mass movement also deposited a sand layer at the site; radionuclide dating and aerial photographs provide independent confirmation that this may have been triggered by intense shaking in 1944 CE during the most recent great Nankai-Suruga megathrust earthquake.
dc.language.isoENen_US
dc.subject.endiatom
dc.subject.enextreme wave event
dc.subject.enlandslide
dc.subject.enpalaeoseismology
dc.subject.enpalynomorph
dc.subject.enradiocarbon
dc.subject.enX-ray computed tomography
dc.title.enHistorical Nankai-Suruga megathrust earthquakes recorded by tsunami and terrestrial mass movement deposits on the Shirasuka coastal lowlands, Shizuoka Prefecture, Japan
dc.typeArticle de revueen_US
dc.identifier.doi10.1177/0959683617752844en_US
dc.subject.halSciences de l'environnement/Milieux et Changements globauxen_US
bordeaux.journalThe Holoceneen_US
bordeaux.page968-983en_US
bordeaux.volume28en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamSEDIMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-02357278
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=The%20Holocene&rft.date=2018-06-01&rft.volume=28&rft.spage=968-983&rft.epage=968-983&rft.eissn=0959-6836&rft.issn=0959-6836&rft.au=GARRETT,%20Edd&FUJIMURA,%20Osamu&RIEDESEL,%20Svenja&WALSTRA,%20Jan&DEFORCE,%20Koen&rft.genre=article


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