Plio-Quaternary stress regime in Esen Cay Basin, SW Turkey

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dc.authoridPINAR, Ali/0000-0002-2641-7344
dc.contributor.authorOver, Semir
dc.contributor.authorÖzden, Süha
dc.contributor.authorYilmaz, Huseyin
dc.contributor.authorPinar, Ali
dc.contributor.authorUnlugenc, Ulvi Can
dc.contributor.authorKamaci, Zuheyr
dc.date.accessioned2025-01-27T20:47:41Z
dc.date.available2025-01-27T20:47:41Z
dc.date.issued2013
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description7th International Symposium on Eastern Mediterranean Geology -- OCT 18-22, 2010 -- Adana, TURKEY
dc.description.abstractThe Plio-Quaternary Esen Cay Basin is situated at the junction of Hellenic and Cyprus arcs in southwestern Turkey. The basin is important for understanding the tectonic evolution of the region in relation to the Hellenic and Cyprus arcs. Fault data from unconsolidated Pliocene and Quaternary deposits, as well as from pre-Pliocene lithologies, are analysed in order to reconstruct the evolution of the stress field evolution from Pliocene onwards. Inversion of measured fault slip vector data identifies two main stress states: extensional and strike-slip. Both states are characterized by a NE-SW-trending minimum horizontal stress axis (sigma(Hmin) = sigma(3)). The mean R value is 0.67, indicating a triaxial state of stress. The inversion also indicates the existence of extensional and strike-slip faulting characterized by a NW-SE-trending sigma(3) axis. This indicates a change in the direction of the minimum horizontal stress axis (sigma(3)) from a NW-SE-trending sigma(3) that dominated prior to Quaternary to a NE-SW-trending sigma(3) that dominated during Quaternary up to actual time.
dc.identifier.doi10.1144/SP372.19
dc.identifier.endpage560
dc.identifier.isbn978-1-86239-353-0
dc.identifier.issn0305-8719
dc.identifier.scopus2-s2.0-84883591468
dc.identifier.scopusqualityQ1
dc.identifier.startpage547
dc.identifier.urihttps://doi.org/10.1144/SP372.19
dc.identifier.urihttps://hdl.handle.net/20.500.12428/25008
dc.identifier.volume372
dc.identifier.wosWOS:000343703000020
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherGeological Soc Publishing House
dc.relation.ispartofGeological Development of Anatolia and The Easternmost Mediterranean Region
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20250125
dc.subjectNorth Anatolian Fault
dc.subjectWestern Anatolia
dc.subjectFocal Mechanisms
dc.subjectEvolution
dc.subjectExtension
dc.subjectState
dc.subjectDeformation
dc.subjectKinematics
dc.subjectSubduction
dc.subjectZone
dc.titlePlio-Quaternary stress regime in Esen Cay Basin, SW Turkey
dc.typeConference Object

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