The morphostructural analysis of the Northern Black Sea shelf

dc.contributor.author	Pedan, Halyna S.
dc.contributor.author	Konikov, Yevhenii G.
dc.contributor.author	Педан, Галина Сергіївна
dc.date.accessioned	2012-04-18T13:04:14Z
dc.date.available	2012-04-18T13:04:14Z
dc.date.issued	2010
dc.description	Caspian-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.abstract	The 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 generation	en
dc.identifier.citation	Black 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.uri	https://dspace.onu.edu.ua/handle/123456789/2370
dc.language.iso	en
dc.subject	shelf	en
dc.subject	Lute Pleistocene	en
dc.subject	Holocene	en
dc.subject	transgression	en
dc.subject	geomorphology structure	en
dc.title	The morphostructural analysis of the Northern Black Sea shelf	en
dc.type	Article	uk

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