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.authoridErginal, Ahmet Evren / 0000-0002-3112-5258en_US
dc.authoridErenoğlu, Ramazan Cüneyt / 000-0002-8212-8379en_US
dc.authoridErenoğlu, Oya / 0000-0003-1235-3009en_US
dc.authoridUlugergerli, Emin / 0000-0001-5639-1109
dc.authorscopusidErginal, Ahmet Evren / 36146986000en_US
dc.authorscopusidErenoğlu, Ramazan Cüneyt / 15836919700en_US
dc.authorscopusidErenoğlu, Oya / 56431151300en_US
dc.authorscopusidUlugergerli, Emin / 6506869477
dc.authorwosidErginal, Ahmet Evren / GCT-8813-2022en_US
dc.authorwosidErenoğlu, Ramazan Cüneyt / ETP-1955-2022en_US
dc.authorwosidErenoğlu, Oya / CPX-2144-2022en_US
dc.contributor.authorErginal, Ahmet Evren
dc.contributor.authorErenoğlu, Ramazan Cüneyt
dc.contributor.authorYıldırım, Cengiz
dc.contributor.authorSelim, H. Haluk
dc.contributor.authorKıyak, Nafiye Güneç
dc.contributor.authorErenoğlu, Oya
dc.contributor.authorUlugergerli, Emin
dc.date.accessioned2023-04-11T07:03:47Z
dc.date.available2023-04-11T07:03:47Z
dc.date.issued2021en_US
dc.departmentFakülteler, Eğitim Fakültesi, Türkçe ve Sosyal Bilimler Eğitimi Bölümü
dc.departmentFakülteler, Mühendislik Fakültesi, Harita Mühendisliği Bölümü
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.citationErginal, A. E., Erenoğlu, R. C., Yıldırım, C., Selim, H. H., Kıyak, N. G., Erenoğlu, O., . . . Karabıyıkoğlu, M. (2021). Co-seismic beachrock deformation of 8th century AD earthquake in middle strand of north anatolian fault, lake iznik, NW turkey. Tectonophysics, 799 doi:10.1016/j.tecto.2020.228690en_US
dc.identifier.doi10.1016/j.tecto.2020.228690
dc.identifier.issn0040-1951
dc.identifier.issn1879-3266
dc.identifier.scopus2-s2.0-85096827834
dc.identifier.urihttps://doi.org/10.1016/j.tecto.2020.228690
dc.identifier.urihttps://hdl.handle.net/20.500.12428/3989
dc.identifier.volume799en_US
dc.identifier.wosWOS:000608866400002
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.institutionauthorErginal, Ahmet Evren
dc.institutionauthorErenoğlu, Ramazan Cüneyt
dc.institutionauthorErenoğlu, Oya
dc.institutionauthorUlugergerli, Emin
dc.language.isoen
dc.publisherElsevieren_US
dc.relation.ispartofTectonophysicsen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.relation.tubitakinfo:eu-repo/grantAgreement/TUBITAK/SOBAG/109Y143
dc.rightsinfo:eu-repo/semantics/closedAccessen_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 Turkey
dc.typeArticle

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