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dc.contributor.authorKöprülü, Kerem
dc.contributor.authorVardar, Denizhan
dc.contributor.authorAlpar, Bedri
dc.date.accessioned2021-03-04T17:48:04Z
dc.date.available2021-03-04T17:48:04Z
dc.date.issued2016
dc.identifier.citationKöprülü K., Alpar B., Vardar D., "Last Glacial - Holocene stratigraphic development at the Marmara Sea exit of the Bosphorus Strait, Turkey", MARINE GEOPHYSICAL RESEARCH, cilt.37, ss.21-35, 2016
dc.identifier.issn0025-3235
dc.identifier.othervv_1032021
dc.identifier.otherav_8756fb3b-3cde-4bda-a8cd-667c5200c267
dc.identifier.urihttp://hdl.handle.net/20.500.12627/91947
dc.identifier.urihttps://doi.org/10.1007/s11001-016-9264-5
dc.description.abstractHigh resolution Chirp and Sparker data allowed definition and mapping of distinct seismic units in the shallow sediment record (similar to 100 ms) acquired from the southern exit of the Bosphorus Strait; a dynamic depositional environment. The bottommost unit observed in the Chirp data (unit-3) is made up of marine-lacustrine sediments thinning seaward and onlaps the basement rocks which are represented by folded strata in the Sparker data, possibly lower to middle Pleistocene age. It is overlain by a series of prograding deposits along the shelf (unit-2) referring to sediment input from the northern sector depending on the water levels of the paleo Marmara lake's during MIS 3. The uppermost deposits (unit-1) close to the Bosphorus Strait were represented by three separate subunits, unlike to relatively thin drape of sediments observed at the other places in the surrounding regions. The detailed definition of these subunits deduced from the closely-spaced reflection profiles and available radiocarbon ages helped to explain the history of the latest stratigraphic development depending on the connections between the Black Sea and the Sea of Marmara. In addition to the previously proposed major conduits, which controlled the sedimentary deposition at the southern exit of the Bosphorus, namely the Bosphorus Strait and Kurbagalidere River, another submarine sedimentary pathway at the eastern bank of the strait's channel seems to have delivered sediments directly into the basin.
dc.language.isoeng
dc.subjectJeofizik Mühendisliği
dc.subjectMühendislik ve Teknoloji
dc.subjectOşinografi
dc.subjectFiziksel Oşinografi
dc.subjectDeniz Bilimleri ve Teknolojisi
dc.subjectOŞİNOGRAFİ
dc.subjectTemel Bilimler (SCI)
dc.subjectYerbilimleri
dc.subjectJEOKİMYA VE JEOFİZİK
dc.titleLast Glacial - Holocene stratigraphic development at the Marmara Sea exit of the Bosphorus Strait, Turkey
dc.typeMakale
dc.relation.journalMARINE GEOPHYSICAL RESEARCH
dc.contributor.department, ,
dc.identifier.volume37
dc.identifier.issue1
dc.identifier.startpage21
dc.identifier.endpage35
dc.contributor.firstauthorID5387


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