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.authorOzden, Suha
dc.contributor.authorYilmaz, Huseyin
dc.contributor.authorPinar, Ali
dc.contributor.authorUnlugenc, Ulvi Can
dc.contributor.authorKamaci, Zuheyr
dc.date.accessioned2024-09-18T21:01:46Z
dc.date.available2024-09-18T21:01:46Z
dc.date.issued2013
dc.departmentHatay Mustafa Kemal Üniversitesien_US
dc.description7th International Symposium on Eastern Mediterranean Geology -- OCT 18-22, 2010 -- Adana, TURKEYen_US
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.en_US
dc.identifier.doi10.1144/SP372.19
dc.identifier.endpage560en_US
dc.identifier.isbn978-1-86239-353-0
dc.identifier.issn0305-8719
dc.identifier.scopus2-s2.0-84883591468en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.startpage547en_US
dc.identifier.urihttps://doi.org/10.1144/SP372.19
dc.identifier.urihttps://hdl.handle.net/20.500.12483/12995
dc.identifier.volume372en_US
dc.identifier.wosWOS:000343703000020en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherGeological Soc Publishing Houseen_US
dc.relation.ispartofGeological Development of Anatolia and The Easternmost Mediterranean Regionen_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectNorth Anatolian Faulten_US
dc.subjectWestern Anatoliaen_US
dc.subjectFocal Mechanismsen_US
dc.subjectEvolutionen_US
dc.subjectExtensionen_US
dc.subjectStateen_US
dc.subjectDeformationen_US
dc.subjectKinematicsen_US
dc.subjectSubductionen_US
dc.subjectZoneen_US
dc.titlePlio-Quaternary stress regime in Esen Cay Basin, SW Turkeyen_US
dc.typeConference Objecten_US

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