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dc.contributor.authorAvşin Görendağlı, Nurcanen_US
dc.contributor.authorVandenberghe, Jefen_US
dc.contributor.authorVan Balen, Ronalden_US
dc.contributor.authorGüneç Kıyak, Nafiyeen_US
dc.contributor.authorÖztürk, Tuğbaen_US
dc.date.accessioned2019-05-05T23:35:16Z
dc.date.available2019-05-05T23:35:16Z
dc.date.issued2019-03
dc.identifier.citationAvsin, N., Vandenberghe, J., van Balen, R., Güneç Kıyak, N. & Öztürk, T. (2019). Tectonic and climatic controls on quaternary fluvial processes and river terrace formation in a mediterranean setting, the goksu river, southern Turkey. Quaternary Research, 91(2), 533-547. doi:10.1017/qua.2018.129en_US
dc.identifier.issn0033-5894
dc.identifier.issn1096-0287
dc.identifier.otherWOS:000464585000006
dc.identifier.urihttps://hdl.handle.net/11729/1584
dc.identifier.urihttp://dx.doi.org/10.1017/qua.2018.129
dc.description.abstractClimate and tectonics effect the fluvial evolution of the Mediterranean Mut basin. The basin contains a river terrace staircase of 16 levels (T16-T1) ranging from 365 to 10m above the current Goksu River in its middle and lower sections. These river terraces records tectonic uplift in the Mut basin. Optically stimulated luminescence (OSL) dating of the fluvial sediments of the youngest terrace (T16) provides a chronology for the assessment of the important impacts of climatic changes. The ages from the youngest river terrace deposits in T16 may be subdivided into two intervals: (1) 239-194.7 ka during the later part of Marine Oxygen Isotope Stage (MIS) 7, implying that the aggradation of T16 started in (the final phase of) this warm period; and (2) 187.9-171 ka during much of MIS 6. Thus, it appears that the Goksu River continued depositing sediment from an interglacial into a glacial time. The differences in climate-driven fluvial evolution between this Mediterranean fluvial system and the classical, well-studied temperate-periglacial river systems in Europe may be the result of different vegetation cover and greater thaw of more intense snowfalls.en_US
dc.language.isoengen_US
dc.publisherCambridge Univ Pressen_US
dc.relation.isversionof10.1017/qua.2018.129
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectRiver terraceen_US
dc.subjectFluvial aggradationen_US
dc.subjectOSL datingen_US
dc.subjectClimate controlen_US
dc.subjectGoksu Riveren_US
dc.subjectTurkeyen_US
dc.subjectEastern Anatoliaen_US
dc.subjectRegional upliften_US
dc.subjectWestern Turkeyen_US
dc.subjectThames valleyen_US
dc.subjectMut basinen_US
dc.subjectEvolutionen_US
dc.subjectSystemsen_US
dc.subjectVegetationen_US
dc.subjectStaircaseen_US
dc.subjectRecorden_US
dc.subjectLuminescenceen_US
dc.subjectTectonicsen_US
dc.subjectMarine oxygen isotopesen_US
dc.subjectOptically stimulated luminescenceen_US
dc.subjectVegetation coveren_US
dc.subjectRiversen_US
dc.subjectRiver terracesen_US
dc.titleTectonic and climatic controls on Quaternary fluvial processes and river terrace formation in a Mediterranean setting, the Goksu River, southern Turkeyen_US
dc.typearticleen_US
dc.description.versionPublisher's Versionen_US
dc.relation.journalQuaternary Research (United States)en_US
dc.contributor.departmentIşık Üniversitesi, Fen Edebiyat Fakültesi, Fizik Bölümüen_US
dc.contributor.departmentIşık University, Faculty of Arts and Sciences, Department of Physicsen_US
dc.contributor.authorID0000-0001-8598-8596
dc.identifier.volume91
dc.identifier.issue2
dc.identifier.startpage533
dc.identifier.endpage547
dc.peerreviewedYesen_US
dc.publicationstatusPublisheden_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.contributor.institutionauthorÖztürk, Tuğbaen_US


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