Evaluation of soil liquefaction in the city of Hatay triggered after the February 6, 2023 Kahramanmaras,-Türkiye earthquake sequence

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dc.authorid0000-0002-1000-1678
dc.authorid0000-0002-2377-8697
dc.authorid0000-0002-9053-1061
dc.contributor.authorBol, Ertan
dc.contributor.authorOzocak, Askin
dc.contributor.authorSert, Sedat
dc.contributor.authorCetin, Kemal Onder
dc.contributor.authorArslan, Eylem
dc.contributor.authorKocaman, Kadir
dc.contributor.authorAyhan, Bilal Umut
dc.date.accessioned2026-04-04T18:55:29Z
dc.date.available2026-04-04T18:55:29Z
dc.date.issued2024
dc.departmentİstanbul Bilgi Üniversitesi
dc.description.abstractThis study investigates the consequences of consequences of liquefaction hazards following the February 6, 2023, Kahramanmaras, Earthquakes in Hatay, T & uuml;rkiye. Field reconnaissance surveys were conducted in areas prone to liquefaction, including recent alluvial basins, the Amik (Amuq) Plain, and the Asi (Orontes) River. Specifically, attention was given to I(center dot)skenderun (Alexandretta), Dortyol coasts, the Hatay Airport region, and Demirkopr & uuml; village near the Asi River. Observations indicated that geological and geomorphological factors primarily influenced liquefaction ejecta and liquefaction-induced lateral spreading in these areas. In Dortyol, liquefaction manifestations were observed on the coastline, which has undergone natural processes, while in I(center dot)skenderun, they occurred on human-made extended reclaimed land. Additionally, liquefaction manifestations in the Hatay Airport region were impacted by the drained Amik Lake, and those in Demirkopr & uuml; Village were influenced by the fluvial nature of the Asi River and its sub facies. The sites experiencing liquefaction and lateral spreading mainly comprised coastal deposits, lacustrine sediments, and sub facies of the meandering river, such as point bars, abandoned channels, and levees. Consequently, the study underscores the significant correlation between geomorphology and liquefaction hazards in the context of the 2023 Kahramanmaras,-T & uuml;rkiye Earthquakes. Considering these factors may facilitate further research and the identification of sites susceptible to liquefaction.
dc.description.sponsorshipScientific and Technological Research Council of Tuerkiye (TUEBITAK)
dc.description.sponsorshipThe authors would like to acknowledge sincere thanks to The Scientific and Technological Research Council of Tuerkiye (TUEBITAK) , for supporting and funding the site investigations with 1002-C Natural Disasters-Focused Fieldwork Emergency investigation program with the project titled 06.02.2023 Kahramanmaras , Earthquakes Evaluation of Geotechnical Problem Areas in Iskenderun-Antakya Region (in Turkish) . In addition, we would like to thank to the Turkish Army officials for providing us video recordings.
dc.identifier.doi10.1016/j.enggeo.2024.107648
dc.identifier.doi10.1016/j.enggeo.2024.107648
dc.identifier.issn0013-7952
dc.identifier.issn1872-6917
dc.identifier.scopus2-s2.0-85199247565
dc.identifier.scopusqualityQ1
dc.identifier.urihttps://doi.org/10.1016/j.enggeo.2024.107648
dc.identifier.urihttps://hdl.handle.net/11411/10442
dc.identifier.volume339
dc.identifier.wosWOS:001279899900001
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherElsevier
dc.relation.ispartofEngineering Geology
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_WoS_20260402
dc.snmzKA_Scopus_20260402
dc.subjectSoil Liquefaction
dc.subjectLateral Spreading
dc.subjectGeomorphological Features
dc.subjectHatay
dc.subject2023 Kahramanmaras ,
dc.subjectT & Uuml;Rkiye Earthquakes
dc.titleEvaluation of soil liquefaction in the city of Hatay triggered after the February 6, 2023 Kahramanmaras,-Türkiye earthquake sequence
dc.typeArticle

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