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dc.contributor.authorKiyak, Nafiye Gunec
dc.contributor.authorErtek, Ahmet
dc.contributor.authorDEMİRCİ, ALPER
dc.contributor.authorEkinci, Yunus Levent
dc.contributor.authorCANEL, TİMUR
dc.contributor.authorErginal, Ahmet Evren
dc.date.accessioned2021-03-03T15:41:16Z
dc.date.available2021-03-03T15:41:16Z
dc.identifier.citationErginal A. E. , Kiyak N. G. , Ekinci Y. L. , DEMİRCİ A., Ertek A., CANEL T., "Age, composition and paleoenvironmental significance of a Late Pleistocene eolianite from the western Black Sea coast of Turkey", QUATERNARY INTERNATIONAL, cilt.296, ss.168-175, 2013
dc.identifier.issn1040-6182
dc.identifier.othervv_1032021
dc.identifier.otherav_404399ca-d23a-4629-8605-285f77e0f2f2
dc.identifier.urihttp://hdl.handle.net/20.500.12627/46975
dc.identifier.urihttps://doi.org/10.1016/j.quaint.2012.04.031
dc.description.abstractOn the basis of field observations, thin section interpretations, microanalytical data, electrical resistivity survey and luminescence dating, the age, composition and internal structure of coastal eolianite on the west Black Sea coast at Sile, Istanbul, was studied for a combined interpretation of dune rock development and facies characteristics. Results demonstrate that the eolianite is made up of south-dipping, large-scale dune stratification, consisting mainly of quartz sand and, in particular, abundant ooids, as well as the binding cement which is composed of calcite and aragonite. Based on Electrical Resistivity Tomography (ERT) images, the eolianite has a thickness of between 3.5 m and 8 m and overlies a buried rugged topography that has developed on the Pliocene unit. This suggests the predominance of northerly winds that account for the landward removal of dune sands by offshore wind drift prior to carbonate cementation. Optically Stimulated Luminescence (OSL) dating estimations revealed that the initial deposition of the laminated eolianite layers on the underlying older unit took place at 138.57 +/- 13.65 ka, matching the Karangatian highstand or Marine Isotope Stage (MIS) 5e. (C) 2012 Elsevier Ltd and INQUA. All rights reserved.
dc.language.isoeng
dc.subjectFiziki Coğrafya
dc.subjectJeoloji Mühendisliği
dc.subjectMühendislik ve Teknoloji
dc.subjectSosyal ve Beşeri Bilimler
dc.subjectCoğrafya
dc.subjectJEOLOJİ
dc.subjectYER BİLİMİ, MULTİDİSİPLİNER
dc.subjectTemel Bilimler (SCI)
dc.subjectYerbilimleri
dc.subjectCOĞRAFYA, FİZİKSEL
dc.titleAge, composition and paleoenvironmental significance of a Late Pleistocene eolianite from the western Black Sea coast of Turkey
dc.typeMakale
dc.relation.journalQUATERNARY INTERNATIONAL
dc.contributor.departmentArdahan Üniversitesi , ,
dc.identifier.volume296
dc.identifier.startpage168
dc.identifier.endpage175
dc.contributor.firstauthorID22464


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