Please use this identifier to cite or link to this item: https://hdl.handle.net/11499/58433
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dc.contributor.authorAkgun, Elif-
dc.contributor.authorTopal, Savas-
dc.contributor.authorSofta, Mustafa-
dc.contributor.authorNas, Murat-
dc.contributor.authorGurgoze, Serkan-
dc.contributor.authorSozbilir, Hasan-
dc.contributor.authorYuksel, Mehmet-
dc.date.accessioned2024-12-21T16:37:15Z-
dc.date.available2024-12-21T16:37:15Z-
dc.date.issued2025-
dc.identifier.issn0191-8141-
dc.identifier.issn1873-1201-
dc.identifier.urihttps://doi.org/10.1016/j.jsg.2024.105293-
dc.descriptionAkgun, Elif/0000-0002-6556-2413; Topal, Savas/0000-0001-7451-6606; Softa, Mustafa/0000-0001-5064-9260en_US
dc.description.abstractThis study examines the unruptured portion of the Puturge segment, the least-studied section of the East Anatolian Fault System (EAFS) in southeast Turkiye, focusing on the S,iro Valley to comprehensively understand the observed distribution in deformation. Despite the February 6, 2023 doublet earthquakes, the Puturge segment near the S,iro Valley remained relatively stable, though significant stress accumulation was detected at both ends. Fieldwork and subsequent morphometric and structural analyses confirmed notable tectonic activity in the area. Geomorphic indices were applied to assess tectonic activity, yielding an average index of relative tectonic activity (Iat) for all drainage basins, highlighting varying tectonic intensity levels across the S,iro Valley. Mountain front sinuosity (Smf) analysis indicated different uplift rates and tectonic forces along distinct fault segments. Additionally, Hypsometric Integral-Hypsometric Curve (HI-HC) index analysis pointed to rapid uplift processes, particularly in the eastern part of the fault-controlled basin, signaling active tectonic uplift and geomorphic rejuvenation. Normalized steepness index (ksn) and Chi (chi) values highlighted variations in erosion rate, providing insight into regional uplift patterns and knickpoint distributions. These findings align with the dominant transtensional tectonic regime in the area, as inferred from slip data inversions along the S,iro Valley. The region's fault geometry, oblique movement, and block rotations firmly support this interpretation. Comparisons of slip rates and ground deformation models revealed notable variations in fault behavior, suggesting ongoing energy accumulation, possibly linked to aseismic creep. The complex fault system behavior was underscored by the 2020 Sivrice earthquake and the 2023 doublet, which highlights the critical role of the Puturge segment in the dynamic evolution of the EAFS.en_US
dc.description.sponsorshipScientific and Technological Research Council of Turkiye (TUBITAK) [122Y266]; TUBITAKen_US
dc.description.sponsorshipThis study was supported by the Scientific and Technological Research Council of Turkiye (TUBITAK) under Grant Number 122Y266. The authors thank TUBITAK for their support.en_US
dc.language.isoenen_US
dc.publisherPergamon-elsevier Science Ltden_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectPuturge Segmenten_US
dc.subjectEast Anatolian Fault Systemen_US
dc.subjectMorphometric Indexen_US
dc.subjectKinematic Analysisen_US
dc.subjectKahramanmaras , Earthquakesen_US
dc.titleEvidence for an Aseismic Gap Between the Mw6.8 Puturge (Elazığ) and 7.8 Pazarcik (Kahramanmaraş) Earthquakes in the East Anatolian Fault System, Southeast Turkiyeen_US
dc.typeArticleen_US
dc.identifier.volume190en_US
dc.departmentPamukkale Universityen_US
dc.authoridAkgun, Elif/0000-0002-6556-2413-
dc.authoridTopal, Savas/0000-0001-7451-6606-
dc.authoridSOFTA, MUSTAFA/0000-0001-5064-9260-
dc.identifier.doi10.1016/j.jsg.2024.105293-
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.authorwosidGürgöze, Serkan/JWA-1776-2024-
dc.authorwosidNas, Murat/AAR-5473-2020-
dc.authorwosidAkgün, Elif/W-5657-2018-
dc.authorwosidSofta, Mustafa/AAH-4566-2019-
dc.authorwosidAksoy, Ercan/GZM-1827-2022-
dc.authorwosidTopal, Savaş/I-1233-2012-
dc.identifier.scopus2-s2.0-85209926252en_US
dc.identifier.scopus2-s2.0-85209926252-
dc.identifier.wosWOS:001396088200001-
dc.institutionauthor-
dc.identifier.scopusqualityQ1-
dc.description.woscitationindexScience Citation Index Expanded-
dc.identifier.wosqualityQ2-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextnone-
item.fulltextNo Fulltext-
item.languageiso639-1en-
item.cerifentitytypePublications-
item.openairetypeArticle-
crisitem.author.dept10.08. Geological Engineering-
Appears in Collections:Mühendislik Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection
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