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dc.contributor.authorDEMİRCİ, ALPER
dc.contributor.authorKARABIYIKOĞLU, MUSTAFA
dc.contributor.authorEKİNCİ, YUNUS LEVENT
dc.contributor.authorOzturk, Tugba
dc.contributor.authorCakir, Caglar
dc.contributor.authorElmas, Elmas Kirci
dc.contributor.authorERGİNAL, AHMET EVREN
dc.contributor.authorKIYAK, NAFİYE GÜNEÇ
dc.contributor.authorSELİM, HAMİT HALUK
dc.contributor.authorBOZCU, MUSTAFA
dc.contributor.authorOzturk, Muhammed Zeynel
dc.date.accessioned2021-03-05T21:42:35Z
dc.date.available2021-03-05T21:42:35Z
dc.identifier.citationERGİNAL A. E. , KIYAK N. G. , SELİM H. H. , BOZCU M., Ozturk M. Z. , EKİNCİ Y. L. , DEMİRCİ A., Elmas E. K. , Ozturk T., Cakir C., et al., "Eolianite and coquinite as evidence of MIS 6 and 5, NW Black Sea coast, Turkey", AEOLIAN RESEARCH, cilt.25, ss.1-9, 2017
dc.identifier.issn1875-9637
dc.identifier.othervv_1032021
dc.identifier.otherav_da3a0406-5c97-4d19-adc8-283d0498d124
dc.identifier.urihttp://hdl.handle.net/20.500.12627/143867
dc.identifier.urihttps://doi.org/10.1016/j.aeolia.2017.01.004
dc.description.abstractThis paper discusses the implications of a lowstand carbonate eolianite and overlying transgressive sequence of coquinite at Sile on the Turkish Black Sea coast based on composition, depositional characteristics and optical age estimations. The cross-bedded eolianite is a mixed ooid quartz grainstone in composition, yielding a depositional age matching MIS 6. It formed at the backshore of the paleobeach with the supply of sediment the from the beach face and offering insights into the drift of mixed shallow marine carbonates and siliciclastics together with radial ooids by onshore winds from a subaerially exposed high- to low-energy ooid shoals and oolitic sand complexes which developed parallel to the shoreline on the shallow shelf margin. During this lowstand, a low-relief dune retaining a record of opposing paleowind directions than that of prevalent northeasterly winds of today appears to have been lithified to form dune rock (aeolinite) under drier conditions compared to the present. Coinciding with MIS 5e, shallow marine coquina beds resting unconformably on the eolianite indicate the occurrence of the Mediterranean transgression during the last interglacial, as confirmed by benthic foraminifera within the high-salinity tolerant coquina shells. (C) 2017 Elsevier B.V. All rights reserved.
dc.language.isoeng
dc.subjectFiziki Coğrafya
dc.subjectCoğrafya
dc.subjectSosyal ve Beşeri Bilimler
dc.subjectTemel Bilimler (SCI)
dc.subjectYerbilimleri
dc.subjectCOĞRAFYA, FİZİKSEL
dc.titleEolianite and coquinite as evidence of MIS 6 and 5, NW Black Sea coast, Turkey
dc.typeMakale
dc.relation.journalAEOLIAN RESEARCH
dc.contributor.departmentİstanbul Üniversitesi , ,
dc.identifier.volume25
dc.identifier.startpage1
dc.identifier.endpage9
dc.contributor.firstauthorID242079


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