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Analyzing the october 16, 2024 mw 5.9 kale (Malatya) earthquake in relation to the february 2023 Kahramanmaraş earthquake sequence and local tectonic dynamics

dc.contributor.authorAlkan, Hamdi
dc.contributor.authorÖztürk, Serkan
dc.contributor.authorBüyüksaraç, Aydın
dc.contributor.buuauthorŞENKAYA, MUSTAFA
dc.contributor.departmentMühendislik Fakültesi
dc.contributor.departmentİnşaat Mühendisliği Ana Bilim Dalı
dc.contributor.orcid0000-0003-3912-7503
dc.contributor.researcheridAAT-1446-2020
dc.date.accessioned2025-10-21T09:20:05Z
dc.date.issued2025-06-19
dc.description.abstractThe 6 February 2023 Mw 7.7-7.6 Kahramanmara & scedil; earthquake sequence has significantly impacted the East Anatolian Fault zone, including the city of Malatya and its immediate surroundings. In addition to the aftershocks of February 2023, the Mw 5.9 Kale earthquake that occurred on October 16, 2024, further underscores the ongoing seismic activity in the region. This study analyzes the distribution of b-values derived from a comprehensive dataset comprising 14,549 earthquakes and the Coulomb stress variations associated with the aftershocks of the February 2023 sequence and the Kale earthquake. The primary objective of this analysis is to enhance the understanding of the tectonic setting that contributed to the occurrence of the Kale earthquake. The findings indicate that the low b-values and stress transfer through the P & uuml;t & uuml;rge segment toward the unnamed fault near Kale are significant contributing factors to the occurrence of the Kale earthquake. Additionally, positive stress variations from Do & gbreve;an & scedil;ehir to Malatya's city center suggest a potential fault oriented toward the city center that may increase the current earthquake hazard. Furthermore, the distribution of seismic events around Malatya suggests a possible barrier supported by previous magnetic data analysis between Malatya and Kale. Lastly, the observed stress variations for the Kale earthquake indicate the likelihood of upcoming seismic events in both the northeast and southwest directions of the Kale.
dc.identifier.doi10.1007/s11600-025-01622-5
dc.identifier.endpage3942
dc.identifier.issn1895-6572
dc.identifier.issue5
dc.identifier.scopus2-s2.0-105008649164
dc.identifier.startpage3923
dc.identifier.urihttps://doi.org/10.1007/s11600-025-01622-5
dc.identifier.urihttps://hdl.handle.net/11452/55966
dc.identifier.volume73
dc.identifier.wos001511659900001
dc.indexed.wosWOS.SCI
dc.language.isoen
dc.publisherSpringer int publ ag
dc.relation.journalActa geophysica
dc.relation.tubitakTUBİTAK
dc.subjectMagnitude-frequency-distribution
dc.subjectAnatolian fault zone
dc.subjectB-values
dc.subjectTurkey
dc.subjectHazard
dc.subject2024 Kale earthquake
dc.subject b -value distribution
dc.subjectStress change
dc.subjectLocal barrier
dc.subjectScience & Technology
dc.subjectPhysical Sciences
dc.subjectGeochemistry & Geophysics
dc.subjectGeochemistry & Geophysics
dc.titleAnalyzing the october 16, 2024 mw 5.9 kale (Malatya) earthquake in relation to the february 2023 Kahramanmaraş earthquake sequence and local tectonic dynamics
dc.typeArticle
dspace.entity.typePublication
local.contributor.departmentMühendislik Fakültesi/İnşaat Mühendisliği Ana Bilim Dalı
local.indexed.atWOS
local.indexed.atScopus
relation.isAuthorOfPublicationcf20d6db-0623-4cc6-80f3-ed914e0887f0
relation.isAuthorOfPublication.latestForDiscoverycf20d6db-0623-4cc6-80f3-ed914e0887f0

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