Please use this identifier to cite or link to this item: http://dspace.onu.edu.ua:8080/handle/123456789/2402
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dc.contributor.authorKonikov, Yevhenii G.-
dc.date.accessioned2012-04-23T11:22:10Z-
dc.date.available2012-04-23T11:22:10Z-
dc.date.issued2006-
dc.identifier.citationBlack sea – mediterranean corridor during the last 30 ky: sea level change and human adaptation (2005–2009) : ІІ plenary meeting and field trip of project IGCP-521 (Odessa, 20–28 August 2006). – Odessa : Astroprint, 2006.uk
dc.identifier.urihttp://dspace.onu.edu.ua:8080/handle/123456789/2402-
dc.descriptionДруга пленарна конференція та польові екскурсії з Проекту IGCP-521 «Чорноморсько-Середземноморський Коридор упродовж останніх 30 тисяч років: мінливість рівня моря й адаптація людини» (2005-2009).Путівник.-Одеса:Астрапринт,2006uk
dc.description.abstractThe accumulative terrace is located on the eastern shore of Berazansky Liman at 1 km from the mouth (Fig.41).The terrace is 1.5-2.0 m in height and 30 m in width.Based on the trenches along the coastal bluff, the following deposits are described after Gozhik (1984):Section 1 (depth, m): 0.00-0.30 modern soil 0.30-1.15 brown-gray sandy mud, diluvial (sharp lower contact) 1.15-1.70 moderately sorted sand with large amounts of Cardium edule, Mytilus sp., and Hydrobia sp. shells (beach facies).The age of shells from this layer is 4500 14C yrs BP.uk
dc.language.isoenuk
dc.publisherAstroprintuk
dc.relation.ispartofseries;C.23-
dc.subjectBerazansky Limanuk
dc.subjectCardium eduleuk
dc.titleRight (western) shore of Berezansky limanuk
dc.typeOtheruk
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