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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.contributor.editorRobertson, AHF
dc.contributor.editorParlak, O
dc.contributor.editorUnlugenc, UC
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T10:00:38Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T10:00:38Z
dc.date.issued2013
dc.identifier.isbn978-1-86239-353-0
dc.identifier.issn0305-8719
dc.identifier.urihttps://dx.doi.org/10.1144/SP372.19
dc.identifier.urihttps://hdl.handle.net/20.500.12418/8812
dc.description7th International Symposium on Eastern Mediterranean Geology -- OCT 18-22, 2010 -- Adana, TURKEYen_US
dc.descriptionWOS: 000343703000020en_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.language.isoengen_US
dc.publisherGEOLOGICAL SOC PUBLISHING HOUSEen_US
dc.relation.ispartofseriesGeological Society Special Publication
dc.relation.isversionof10.1144/SP372.19en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.titlePlio-Quaternary stress regime in Esen Cay Basin, SW Turkeyen_US
dc.typeconferenceObjecten_US
dc.relation.journalGEOLOGICAL DEVELOPMENT OF ANATOLIA AND THE EASTERNMOST MEDITERRANEAN REGIONen_US
dc.contributor.department[Over, Semir] Mustafa Kemal Univ, Dept Geophys Engn, TR-31040 Antakya, Turkey -- [Ozden, Suha] Canakkale Onsekiz Mart Univ, Dept Geol Engn, TR-17020 Canakkale, Turkey -- [Yilmaz, Huseyin] Cumhuriyet Univ, Dept Geophys Engn, TR-58140 Sivas, Turkey -- [Pinar, Ali] Bogazici Univ, Kandilli Observ, TR-34684 Istanbul, Turkey -- [Pinar, Ali] Bogazici Univ, Earthquake Res Inst, TR-34684 Istanbul, Turkey -- [Unlugenc, Ulvi Can] Cukurova Univ, Dept Geol Engn, TR-01330 Adana, Turkey -- [Kamaci, Zuheyr] Suleyman Demirel Univ, Dept Geophys Engn, TR-32260 Isparta, Turkeyen_US
dc.contributor.authorIDPINAR, Ali -- 0000-0002-2641-7344en_US
dc.identifier.volume372en_US
dc.identifier.endpage560en_US
dc.identifier.startpage547en_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US


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