Main Regularities of the Late Pleistocene–Holocene Transgression of the Black Sea

dc.contributor.authorEsin, Nikolay V.
dc.contributor.authorYanko-Hombach, Valentyna V.
dc.contributor.authorKuklevaa, O. N.
dc.contributor.authorEsin, Nikolay I.
dc.contributor.authorЯнко-Хомбах, Валентина Венедиктовна
dc.contributor.authorЯнко-Хомбах, Валентина Венедиктівна
dc.contributor.authorЕсин, Николай В.
dc.contributor.authorЕсин, Николай Игоревич
dc.contributor.authorЄсін, Микола Ігорович
dc.contributor.authorЄсін, Микола В.
dc.contributor.authorКуклева, О. Н.
dc.date.accessioned2018-11-08T09:37:52Z
dc.date.available2018-11-08T09:37:52Z
dc.date.issued2010
dc.description.abstractA mathematical model describing the Black Sea level change in the Late Pleistocene–Holocene is offered. A theoretical curve for temporal change in the sea level is obtained. It is established that, in the range from 20 to 12 ky BP, the sea level rose to ~20 m and fluctuated with various amplitudes and periods. In the range from 12 to 11 ky BP during the Bosphorus Strait formation, there was a sea regression by 30– 50 meters, and level of the Black Sea dropped to the World Ocean level. Further, it mirrored variation of the ocean level.uk
dc.identifierDOI: 10.1134/S1028334X10020108
dc.identifier.citationDoklady Earth Sciencesuk
dc.identifier.urihttps://dspace.onu.edu.ua/handle/123456789/19428
dc.language.isoenuk
dc.publisherPleiades Publishing, Ltd.uk
dc.relation.ispartofseries;Vol. 430, Part 2
dc.subjectBlack Seauk
dc.subjectMain Regularitiesuk
dc.subjectLate Pleistoceneuk
dc.subjectHolocene Transgressionuk
dc.titleMain Regularities of the Late Pleistocene–Holocene Transgression of the Black Seauk
dc.typeArticleuk
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