Paleoseismological features and tectonic setting of the Fethiye-Burdur Fault Zone (SW Turkey)

dc.contributor.authorSari, Coşkun
dc.contributor.authorKamaci, Züheyr
dc.contributor.authorYağmurlu, Fuzulİ
dc.contributor.authorTİmur, Emre
dc.contributor.authorŞentürk, Murat
dc.contributor.authorBozcu, Mustafa
dc.date.accessioned2025-01-27T18:59:01Z
dc.date.available2025-01-27T18:59:01Z
dc.date.issued2023
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractThe Fethiye-Burdur fault zone is not a single line. Still, it consists of discontinuous northeasterly trending fault segments developed parallel to each other between the Gulf of Fethiye and Burdur Lake. The NE-trending and left-lateral oblique-slip Fethiye-Burdur fault zone bounds the Isparta Angle to the west and is probably a continuation of the Pliny fault zone of the Hellenic arc. Year 1914, 1957, and 1971 earthquakes occurred in the Fethiye-Burdur fault zone, with magnitudes of 7.1, 7.0, and 6.1, respectively. The epicenter distribution of the earthquakes of the last century indicates the continuation of the Fethiye-Burdur fault zone under the Gulf of Fethiye, probably to Rhodos Island. According to GPS measurements, the Fethiye-Burdur fault zone is the southern limit of the Aegean extensional region. The Aegean region is characterized by coherent motion toward the SW at 30 mm/yr relative to the Eurasian plate. Field observations and fault plane solutions of recent earthquakes in and around the Burdur Lake region reflect normal and left-lateral oblique faulting considering the NE extension of the fault zone. According to the proposed kinematic model, the different seismotectonic behaviors of the Fethiye-Burdur fault zone originate in the rigid influence of Yeşilova peridotite massif of the Lycian nappes that occur to the SW of Burdur Lake. The kinematic interactions between the mainly NE-trending enechelon fault constituents of the Fethiye-Burdur fault zone result in different seismotectonic characteristics. Consequently, a new kinematic model is obtained for Burdur Lake and its surroundings. © (2023), (University of Belgrade). All Rights Reserved.
dc.description.sponsorshipTurkish Council for Scientific and Technical Research; Turkish Council for Scientific and Tech? nical Research; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu, TÜBİTAK; Süleyman Demirel Üniversitesi, SDÜ
dc.identifier.doi10.2298/GABP230529009S
dc.identifier.endpage131
dc.identifier.issn0350-0608
dc.identifier.issue2
dc.identifier.scopus2-s2.0-85185336995
dc.identifier.scopusqualityQ3
dc.identifier.startpage117
dc.identifier.urihttps://doi.org/10.2298/GABP230529009S
dc.identifier.urihttps://hdl.handle.net/20.500.12428/13121
dc.identifier.volume84
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherUniversity of Belgrade
dc.relation.ispartofGeoloski Anali Balkanskoga Poluostrva
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_Scopus_20250125
dc.subjectfault-plane solutions; Fethiye-Burdur fault zone; seismicity; seismotectonic
dc.titlePaleoseismological features and tectonic setting of the Fethiye-Burdur Fault Zone (SW Turkey)
dc.title.alternative???????????????? ?????????????? ? ????????? ???????? ??????? ???? Fethiye-Burdur (?? ??????)
dc.typeArticle

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