Please use this identifier to cite or link to this item: http://dspace.onu.edu.ua:8080/handle/123456789/2370
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dc.contributor.authorPedan, Halyna S.-
dc.contributor.authorKonikov, Yevhenii G.-
dc.contributor.authorПедан, Галина Сергіївна-
dc.date.accessioned2012-04-18T13:04:14Z-
dc.date.available2012-04-18T13:04:14Z-
dc.date.issued2010-
dc.identifier.citationBlack sea-mediterranean corridor during the last 30 ky: sea level change and human adaptation (2005–2010) : VI plenarry meeting and field trip IGCP-521 (Rhodes, 27 Sept. – 5 Oct., 2010). – Rhodes, 2010.uk
dc.identifier.urihttp://dspace.onu.edu.ua:8080/handle/123456789/2370-
dc.descriptionCaspian-Black Sea-mediterranean corridor during last 30 ky: sea level change and human adaptiv strategies (2005-2011), plenary meeting and field trip INQUA 501 (6,2010),27 Sept.-5 Oct., 2010-
dc.description.abstractThe Northern Black Sea shelf is a subaerial plain and regional zone of the continental platform. It is a classic example of a transgression-regression shelf. During the Late Pleistocene and Holocene, the shelf was flooded and drained repeatedly as the coastline migrated across its surface (Shcherbakov et al., 1976; Ivanov et al., 1982). According to Morgunov et al. (1981), the modern relief of the coastal part of the shelf is a zone of flooded valleys of late generationen
dc.language.isoen-
dc.subjectshelfen
dc.subjectLute Pleistoceneen
dc.subjectHoloceneen
dc.subjecttransgressionen
dc.subjectgeomorphology structureen
dc.titleThe morphostructural analysis of the Northern Black Sea shelfen
dc.typeArticleuk
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