Fluvio-karstic evolution of the Taseli Plateau (Central Taurus, Turkey)

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dc.authoridOzturk, Muhammed Zeynel/0000-0002-9834-7680
dc.contributor.authorOzturk, Muhammed Zeynel
dc.date.accessioned2024-11-07T13:25:17Z
dc.date.available2024-11-07T13:25:17Z
dc.date.issued2020
dc.departmentNiğde Ömer Halisdemir Üniversitesi
dc.description.abstractUplift history is an important factor in the structural patterns and karstification of the Taseli Plateau. The morphological development of the study area consists of five stages according to its sedimentation, rotation, uplift, and climatic properties. (1) Shallow carbonates accumulated during the Early Miocene. (2) An emersion and drainage network developed as a result of the compressional neotectonic regime in the Late Miocene. (3) Dense joint systems were formed due to the similar to 40 degrees clockwise rotation of the eastern limb of the Isparta Angle. (4) The climate of the study area changed as a result of rapid uplift from Late Pliocene to Early Pleistocene. This caused the formation of dry valleys, underground karstification on the plateau surface, and headward erosion of rivers in the southern part of the area. (5) In the last stage, the plateau surface was densely covered by solution dolines and the dry valley network turned into relict valleys due to expanding extensional cracks during Pleistocene.
dc.description.sponsorshipScientific and Technological Research Council of Turkey (TUBITAK) [115Y580]
dc.description.sponsorshipThis study was financially supported by the Scientific and Technological Research Council of Turkey (TUBITAK) (Project no: 115Y580). I express my sincere gratitude to Mehmet Furkan Sener, Mesut Simsek, Mustafa Utlu, and Murat Poyraz for their assistance in the field studies. I also thank Graham H. Lee for checking the English of the paper.
dc.identifier.doi10.3906/yer-1908-1
dc.identifier.endpage746
dc.identifier.issn1300-0985
dc.identifier.issue5
dc.identifier.scopus2-s2.0-85087424271
dc.identifier.scopusqualityQ2
dc.identifier.startpage733
dc.identifier.trdizinid354394
dc.identifier.urihttps://doi.org/10.3906/yer-1908-1
dc.identifier.urihttps://search.trdizin.gov.tr/tr/yayin/detay/354394
dc.identifier.urihttps://hdl.handle.net/11480/14622
dc.identifier.volume29
dc.identifier.wosWOS:000545784400003
dc.identifier.wosqualityQ4
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.indekslendigikaynakTR-Dizin
dc.language.isoen
dc.publisherTubitak Scientific & Technological Research Council Turkey
dc.relation.ispartofTurkish Journal of Earth Sciences
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_20241106
dc.subjectSolution doline
dc.subjectrelict valley
dc.subjectTaseli Plateau
dc.subjectTaurus Mountains
dc.titleFluvio-karstic evolution of the Taseli Plateau (Central Taurus, Turkey)
dc.typeArticle

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