Tectonic implications of the February 2023 Earthquakes (Mw7.7, 7.6 and 6.3) in south-eastern Turkiye

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dc.authoridDemirci, Alper/0000-0002-8710-6232
dc.contributor.authorOver, Semir
dc.contributor.authorDemirci, Alper
dc.contributor.authorÖzden, Süha
dc.date.accessioned2025-01-27T20:12:24Z
dc.date.available2025-01-27T20:12:24Z
dc.date.issued2023
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractThe series of earthquakes that took place on February 6, 2023 caused one of the saddest major calamities in Turkiye. The first major earthquake of magnitude Mw7.7 broke the Pazarcik and Erkenek segments moving north on the East Anatolian Fault Zone (EAFZ) between Turkoglu and celikhan. According to the Coulomb failure criterion, the Pazarcik earthquake (Mw7.7) increased stress on the Surgu-cardak Fault, a segment on the north splay of the EAFZ, and nine hours later the Elbistan earthquake (Mw7.6) occurred. This great event ruptured the cardak Fault, the western part of the E-W trending Surgu-cardak Fault between Nurhak and Goksun. The Amanos Fault, which extends from Turkoglu south to Antakya, broke almost simultaneously to the first Pazarcik earthquake. Similarly, the earthquake that broke the Amanos Fault transferred increased stress to its southwestern neighbour, the Cyprus-Antakya Transform Fault, triggering the 6.3 magnitude Samandag earthquake 14 days later. The February 2023 earthquakes, which caused the collapse of >100,000 buildings and the death of >50,000 people, created surface ruptures hundreds of kilometres in length and caused different displacements on different faults, the two largest of which were 4.6 and 6.7 m. On all the faults where the deadly earthquakes occurred in February 2023, inversion of the focal mechanisms of the earthquakes (main shocks and their aftershocks) indicates a transtensional stress regime, or a change from strike-slip to normal slip. For all strike-slip inversions, the R values are <0.45 indicating transtension. The stress tensors obtained indicate left-lateral movement with normal component on all faults where the earthquakes occurred. The transtensional regime, which is thought to reflect regional tectonics, is the result of forces caused by relative movements of Arabia, eastern Mediterranean and Eurasia.
dc.identifier.doi10.1016/j.tecto.2023.230058
dc.identifier.issn0040-1951
dc.identifier.issn1879-3266
dc.identifier.scopus2-s2.0-85172992011
dc.identifier.scopusqualityQ1
dc.identifier.urihttps://doi.org/10.1016/j.tecto.2023.230058
dc.identifier.urihttps://hdl.handle.net/20.500.12428/20932
dc.identifier.volume866
dc.identifier.wosWOS:001092109800001
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherElsevier
dc.relation.ispartofTectonophysics
dc.relation.publicationcategoryinfo:eu-repo/semantics/openAccess
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20250125
dc.subjectKahramanmaras , Earthquakes
dc.subjectStress Tensor Inversion
dc.subjectTranstension
dc.subjectEast Anatolian Fault
dc.subjectS-SE Turkiye
dc.subjectEastern Mediterranean Domain
dc.titleTectonic implications of the February 2023 Earthquakes (Mw7.7, 7.6 and 6.3) in south-eastern Turkiye
dc.typeArticle

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