Paleoseismology of the Surgu and cardak faults-splays of the Eastern Anatolian Fault Zone, Turkiye

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dc.authorid0000-0001-6321-0812en_US
dc.authorscopusid7005349357en_US
dc.authorwosid-en_US
dc.contributor.authorBalkaya, Musa
dc.contributor.authorAkyüz, Hüsnü Serdar
dc.contributor.authorÖzden, Süha
dc.date.accessioned2024-01-23T11:39:08Z
dc.date.available2024-01-23T11:39:08Z
dc.date.issued2023en_US
dc.departmentFakülteler, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü
dc.description.abstractThe sinistral East Anatolian Fault Zone (EAFZ) and the dextral North Anatolian Fault Zone (NAFZ) are two important strike-slip faults that delimit the boundaries of the Anatolian plate. The north-south directed compressional forces in eastern Türkiye trigger the westward escape of the Anatolian plate along these prominent structures. This study aims to reveal the earthquake history of the Sürgü and Çardak faults, which are important fault segments that splay from the EAFZ. In this context, overall, four paleoseismologic trenches were dug, two trenches on the Sürgü Fault and two trenches on the Çardak Fault. Along the Sürgü Fault, at least two paleoearthquake events have been determined on the trench walls, one event occurred around 3400 BCE and the second event happened between 2085 ± 65 BCE and 790 ± 20 BCE. Moreover, trenching results from the Çardak Fault indicate two surface rupturing paleoearthquakes between 10520 ± 95 BCE and 5780 ± 65 BCE, and between 3215 ± 125 BCE and 825 ± 55 CE, respectively. The focal mechanisms of important instrumental earthquakes around the Sürgü and Çardak faults on the EAFZ show that NNE-SSW trending compressional forces are actively dominating the tectonic setting of the region in the contemporary era. Paleoseismological investigations suggested that the Sürgü and Çardak faults have the potential to produce surface-rupturing earthquakes with an estimated magnitude of 7 or larger.en_US
dc.identifier.citationBalkaya, M., Akyüz, H., Özden, S. (2023). Paleoseismology of the Sürgü and Çardak faults—splays of the Eastern Anatolian Fault Zone, Türkiye. Turkish Journal of Earth Sciences, 32(SI-3), 402 - 420. doi: 10.55730/1300-0985.1851en_US
dc.identifier.doi10.55730/1300-0985.1851
dc.identifier.endpage420en_US
dc.identifier.issn1300-0985
dc.identifier.issueSI-3en_US
dc.identifier.scopus2-s2.0-85160024666
dc.identifier.startpage402en_US
dc.identifier.trdizinid1180351
dc.identifier.urihttps://doi.org/10.55730/1300-0985.1851
dc.identifier.urihttps://hdl.handle.net/20.500.12428/5348
dc.identifier.volume32en_US
dc.identifier.wosWOS:000991004800010
dc.identifier.wosqualityQ4
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.indekslendigikaynakTR-Dizin
dc.institutionauthorÖzden, Süha
dc.language.isoen
dc.publisherTUBITAKen_US
dc.relation.ispartofTurkish Journal of Earth Sciencesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.relation.tubitakinfo:eu-repo/grantAgreement/TUBITAK/SOBAG/120Y102
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.subjectEarthquakeen_US
dc.subjectEast Anatolian Fault Zoneen_US
dc.subjectPaleoseismologyen_US
dc.subjectSE Türkiyeen_US
dc.titlePaleoseismology of the Surgu and cardak faults-splays of the Eastern Anatolian Fault Zone, Turkiye
dc.typeArticle

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