Neogene-Quaternary evolution of the Tefenni basin on the Fethiye-Burdur fault zone, SW Anatolia-Turkey

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dc.contributor.authorAksoy, Rahmi
dc.contributor.authorAksarı, Süleyman
dc.date.accessioned2020-03-26T19:25:16Z
dc.date.available2020-03-26T19:25:16Z
dc.date.issued2016
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractThe Fethiye-Burdur fault zone (FBFZ) is a complex belt of major break in the southwestern Anatolia. A number of basins occur within the FBFZ. The Tefenni basin is one of the NE-SW trending basins located in the central part of the FBFZ. The basin is 10-20 km wide and 60 km long. It contains two infills of fluvial, lacustrine and alluvial fan deposits from late Miocene to Recent. The older and folded infill rests on the pre-middle Miocene basement rocks with an angular unconformity and consists of fluvial and lacustrine sediments. The younger and undeformed Plio-Quaternary basin fill unconformably overlies the older basin fill and is composed predominantly of conglomerate, mudstone, silt, clay and recent basin floor sediments. The Tefenni basin is controlled by a series of NE-SW trending left lateral oblique-slip normal faults along its margins. The Tefenni and Murseller faults bound the northwestern margin of the basin and the Kemer fault bounds the southeastern margin of the basin. The basin is also cut by NE-SW striking major and NW-SE, N-S and E-W striking small scale normal faults. Structural analyses in the basin show that NE-SW-trending contraction stress regime ended by Pliocene and was followed by NE-SW-trending extension from Pliocene onward. (C) 2016 Elsevier Ltd. All rights reserved.en_US
dc.identifier.doi10.1016/j.jafrearsci.2016.02.024en_US
dc.identifier.endpage148en_US
dc.identifier.issn1464-343Xen_US
dc.identifier.issn1879-1956en_US
dc.identifier.scopusqualityQ2en_US
dc.identifier.startpage137en_US
dc.identifier.urihttps://dx.doi.org/10.1016/j.jafrearsci.2016.02.024
dc.identifier.urihttps://hdl.handle.net/20.500.12395/33817
dc.identifier.volume118en_US
dc.identifier.wosWOS:000378434500012en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherPERGAMON-ELSEVIER SCIENCE LTDen_US
dc.relation.ispartofJOURNAL OF AFRICAN EARTH SCIENCESen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectFethiye-Burdur fault zoneen_US
dc.subjectTefenni basinen_US
dc.subjectNeogene-Quaternaryen_US
dc.subjectKinematic analysisen_US
dc.subjectWestern Anatoliaen_US
dc.titleNeogene-Quaternary evolution of the Tefenni basin on the Fethiye-Burdur fault zone, SW Anatolia-Turkeyen_US
dc.typeArticleen_US

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