Genetic framework of Neogene-Quaternary basin closure process in central Turkey

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dc.contributor.authorGurbuz, Alper
dc.contributor.authorKazanc, Nizamettin
dc.date.accessioned2019-08-01T13:38:39Z
dc.date.available2019-08-01T13:38:39Z
dc.date.issued2015
dc.departmentNiğde ÖHÜ
dc.description.abstractCentral Turkey represents the only orogenic plateau in the Mediterranean region. Also, the largest closed drainage basin and the largest intracontinental basin of Turkey, the Lake Tuz Basin, is located in this region. Results from a three-dimensional (3-D) computer modeling study of the Lake Tuz Basin indicate a southward-deepening freshwater lake basin with great depth in the Mio-Pliocene, which regressed toward the north during the Plio-Quaternary into the shallow saline lake basin it is today. The spatio-temporal variations of Neogene and Quaternary deposits reflect the main effects of internal forces (isostasy>volcanism>faulting) that were caused by lithospheric slab breakoff and subsequent asthenospheric upwelling under central Turkey. Climatic change played a relatively minor role during these periods and was closely associated with the results of internal forces.
dc.description.sponsorshipAUBAP (Ankara University Scientific Research Projects) [09B4343017]
dc.description.sponsorshipWe are grateful to I.O. Yilmaz, G. Seyitoglu, O.F. Gurer, B. Varol, Y.K. Kadioglu, A. Ates, F. Saroglu, and L. Royden for their contributions and fruitful discussions. The constructive reviews of E. Kirby, Y. Dilek, and T. Schildgen improved the manuscript significantly. This study was supported by the AUBAP (Ankara University Scientific Research Projects, Grant no: 09B4343017).
dc.identifier.doi10.1130/L408.1
dc.identifier.endpage426
dc.identifier.issn1941-8264
dc.identifier.issn1947-4253
dc.identifier.issue4
dc.identifier.scopus2-s2.0-84938572136
dc.identifier.scopusqualityQ2
dc.identifier.startpage421
dc.identifier.urihttps://dx.doi.org/10.1130/L408.1
dc.identifier.urihttps://hdl.handle.net/11480/3897
dc.identifier.volume7
dc.identifier.wosWOS:000359000300005
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.institutionauthor[0-Belirlenecek]
dc.language.isoen
dc.publisherGEOLOGICAL SOC AMER, INC
dc.relation.ispartofLITHOSPHERE
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleGenetic framework of Neogene-Quaternary basin closure process in central Turkey
dc.typeArticle

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