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dc.rights.licenseopenen_US
dc.contributor.authorHUBERT-FERRARI, Aurélia
dc.contributor.authorEL-OUAHABI, Meriam
dc.contributor.authorGARCIA-MORENO, David
dc.contributor.authorAVŞAR, Ulaş
dc.contributor.authorALTINOK, Sevgi
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
dc.contributor.authorFAGEL, Nathalie
dc.contributor.authorÇAĞATAY, M. Namık
dc.date.accessioned2024-06-13T12:43:10Z
dc.date.available2024-06-13T12:43:10Z
dc.date.issued2017-04-03
dc.identifier.issn0037-0746en_US
dc.identifier.uriorcid:0000-0002-5985-9747:10.1111/sed.12355
dc.identifier.urioai:crossref.org:10.1111/sed.12355
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200462
dc.description.abstractEnDeltas contain sedimentary records that are not only indicative of water-level changes, but also particularly sensitive to earthquake shaking typically resulting in soft-sediment-deformation structures. The Kürk lacustrine delta lies at the south-western extremity of Lake Hazar in eastern Turkey and is adjacent to the seismogenic East Anatolian Fault, which has generated earthquakes of magnitude 7. This study re-evaluates water-level changes and earthquake shaking that have affected the Kürk Delta, combining geophysical data (seismic-reflection profiles and side-scan sonar), remote sensing images, historical data, onland outcrops and offshore coring. The history of water-level changes provides a temporal framework for the depositional record. In addition to the common soft-sediment deformation documented previously, onland outcrops reveal a record of deformation (fracturing, tilt and clastic dykes) linked to large earthquake-induced liquefactions and lateral spreading. The recurrent liquefaction structures can be used to obtain a palaeoseismological record. Five event horizons were identified that could be linked to historical earthquakes occurring in the last 1000 years along the East Anatolian Fault. Sedimentary cores sampling the most recent subaqueous sedimentation revealed the occurrence of another type of earthquake indicator. Based on radionuclide dating (137Cs and 210Pb), two major sedimentary events were attributed to the ad 1874 to 1875 East Anatolian Fault earthquake sequence. Their sedimentological characteristics were determined by X-ray imagery, X-ray diffraction, loss-on-ignition, grain-size distribution and geophysical measurements. The events are interpreted to be hyperpycnal deposits linked to post-seismic sediment reworking of earthquake-triggered landslides.
dc.language.isoENen_US
dc.sourceorcid
dc.sourcecrossref
dc.title.enEarthquake imprints on a lacustrine deltaic system: The Kürk Delta along the East Anatolian Fault (Turkey)
dc.typeArticle de revueen_US
dc.identifier.doi10.1111/sed.12355en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalSedimentologyen_US
bordeaux.page1322-1353en_US
bordeaux.volume64en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue5en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamSEDIMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04611099
hal.version1
hal.date.transferred2024-06-13T12:43:16Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Sedimentology&rft.date=2017-04-03&rft.volume=64&rft.issue=5&rft.spage=1322-1353&rft.epage=1322-1353&rft.eissn=0037-0746&rft.issn=0037-0746&rft.au=HUBERT-FERRARI,%20Aur%C3%A9lia&EL-OUAHABI,%20Meriam&GARCIA-MORENO,%20David&AV%C5%9EAR,%20Ula%C5%9F&ALTINOK,%20Sevgi&rft.genre=article


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