Co-seismic beachrock deformation of 8th century AD Earthquake in Middle Strand of North Anatolian Fault, Lake Iznik, NW Turkey

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dc.authoridhttps://orcid.org/0000-0001-5253-028Xen_US
dc.contributor.authorErginal, Ahmet Evren
dc.contributor.authorErenoğlu, Ramazan Cüneyt
dc.contributor.authorYıldırım, Cengiz
dc.contributor.authorSelim, Hamit Haluk
dc.contributor.authorKıyak, Nafiye Güneç
dc.contributor.authorErenoğlu, Oya
dc.contributor.authorUlugergerli, Emin
dc.contributor.authorKarabıyıkoğlu, Mustafa
dc.date.accessioned2023-06-19T17:00:47Z
dc.date.available2023-06-19T17:00:47Z
dc.date.issued2021en_US
dc.departmentMühendislik ve Mimarlık Fakültesien_US
dc.description.abstractA historical earthquake-related co-seismic deformation observed on beachrock beds along the southern shoreline of Lake Iznik is discussed as a new paleoseismic record for an 8th century AD earthquake in the Middle Strand of the North Anatolian Fault, NW Turkey. Electrical Resistivity Tomography (ERT) images beneath the beachrock surface allowed monitoring of the subsurface trace of a normal fault dipping north along a 100 m surface rupture. No strike-slip deformation exists along the rupture, suggesting that the deformation in the beachrock is connected with a secondary structure, and that the main surface rupture was under the lake waters. The deformed beds of the beachrock, dated using Optically Stimulated Luminescence (OSL) to 1.3 ± 0.15 ka, are overlain by an undeformed secondary deposition of beds dated to 1.2 ± 0.09 ka. This allows us to narrow down the time of the faulting and implying that it was most likely a result of the AD 715 earthquake.en_US
dc.identifier.doi10.1016/j.tecto.2020.228690en_US
dc.identifier.endpage8en_US
dc.identifier.issn0040-1951
dc.identifier.issn1879-3266
dc.identifier.scopus2-s2.0-85096827834en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.startpage1en_US
dc.identifier.urihttps://hdl.handle.net/11363/4904
dc.identifier.urihttps://doi.org/
dc.identifier.volume799en_US
dc.identifier.wosWOS:000608866400002en_US
dc.identifier.wosqualityQ2en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.institutionauthorSelim, Hamit Haluk
dc.language.isoenen_US
dc.publisherELSEVIER, RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDSen_US
dc.relation.ispartofTectonophysicsen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectNorth Anatolian Faulten_US
dc.subjectMiddle Stranden_US
dc.subjectLake Izniken_US
dc.subjectPaleoseismologyen_US
dc.subjectAD 715en_US
dc.subjectBeachrocken_US
dc.titleCo-seismic beachrock deformation of 8th century AD Earthquake in Middle Strand of North Anatolian Fault, Lake Iznik, NW Turkeyen_US
dc.typeArticleen_US

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