Late Cenozoic stress states in the Datça and Bozburun Peninsulas, SE Aegean, Turkey

Basit Öğe Kaydı
dc.authorid0000-0002-6836-2951
dc.authorid0000-0002-8710-6232
dc.contributor.authorDemirci, Alper
dc.contributor.authorOzden, Suha
dc.contributor.authorOver, Semir
dc.contributor.authorGundogdu, Erdem
dc.date.accessioned2026-02-03T12:00:07Z
dc.date.available2026-02-03T12:00:07Z
dc.date.issued2025
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractThe Datpa and Bozburun are E-W-oriented peninsulas located near the Pliny-Strabo Trench Zone and considered to be eastern continuations of the seismically-active Hellenic Subduction Zone. Although no catastrophic earthquakes were recorded on the peninsulas in the previous century, two large earthquakes of a magnitude of 6.6 (Mw) occurred in the Gulf of G & ouml;kova in the north, in 2017, and a magnitude of 7.1 (Mw) in the Gulf of Fethiye in the south was recorded in 1957. Therefore, the necessity to pay close attention and issue warnings regarding potential earthquakes in and around the peninsulas has been increasing. Inversion of fault slip vectors affecting both the Plio-Quaternary and Paleozoic units in the Datpa and Bozburun Peninsulas yields N-S, NE-SW, and NW-SE extensional stress states. The NW-SE trending Datpa Basin formed during the Plio-Quaternary under the NE-SW extensional regime. The inversion of the focal mechanisms for shallow earthquakes in the Datpa and Bozburun Peninsulas provides N-S and NW-SE extensional stress states. Extensional stress tensors obtained from both the fault planes measured, as well as the focal mechanisms of the shallow earthquakes, are related to the roll-back process of the African slab along the Hellenic Subduction Zone.
dc.description.sponsorshipCOMUE-BAP [FHD-2021-3736]
dc.description.sponsorshipAcknowledgements: This study was supported by COMU-BAP (FHD-2021-3736) as a research project. The authors would like to thank Catherine Yi & gbreve;it for professional editing assistance with English exposition that improved the latest version of the text. We also thank the editor and anonymous reviewers for their valuable comments and suggestions, which improved the overall quality of the manuscript.
dc.identifier.doi10.31577/GeolCarp.2025.06
dc.identifier.endpage136
dc.identifier.issn1335-0552
dc.identifier.issn1336-8052
dc.identifier.issue2
dc.identifier.scopus2-s2.0-105015166791
dc.identifier.scopusqualityQ2
dc.identifier.startpage117
dc.identifier.urihttps://doi.org/10.31577/GeolCarp.2025.06
dc.identifier.urihttps://hdl.handle.net/20.500.12428/34518
dc.identifier.volume76
dc.identifier.wosWOS:001597965700003
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherSlovak Acad Sciences, Earth Science Inst
dc.relation.ispartofGeologica Carpathica
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_WOS_20260130
dc.subjectDatpa and Bozburun Peninsulas
dc.subjectlate Cenozoic stress states
dc.subjectextensional
dc.subjectHellenic Subduction Zone
dc.titleLate Cenozoic stress states in the Datça and Bozburun Peninsulas, SE Aegean, Turkey
dc.typeArticle

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