The processes of the Caspian-Mediterranean corridor formation and the Paratethys Sa-Lake degradation

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dc.contributor.authorEsin, Nikolay V.
dc.contributor.authorEsin, Nikolay I.
dc.contributor.authorYanko-Hombach, Valentyna V.
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.date.accessioned2018-11-08T09:57:36Z
dc.date.available2018-11-08T09:57:36Z
dc.date.issued2015
dc.description.abstractIt is known that about 14 million years ago, a division of the Tethys Ocean occurred into the Mediterranean Sea and the Sea-Lake of the Paratethys. During the next 10 million years, its water area decreased in size, the sea-lake became shallow, and eventually subdivided into the Azov, Black, and Caspian seas. The first stage of the Paratethys closure was the Sarmatian Sea-Lake (14.0-10.5 million years ago). The initial water was salty as in the ocean. Then, as a result of the large inflow of freshwater, there was a Ireshening of the sea water. During Meotian time (10.5-7.0 million years ago), the Mediterranean salt water got into the sea-lake. Then, there was water desalination in the Meotian Sea. During this entire period, the level of the sea-lake changed with a trend towards a decreasing level. .Approximately 6-5 million years ago, in the Balakhanian stage (the beginning of the Pliocene), the sea- lake level decreased significantly, and it separated into the Black and Caspian seas.uk
dc.identifier.citationIGCP 610 Third Plenary Conference and Field Trip. Astrakhan. Russia, 22-30 September, 2015uk
dc.identifier.urihttps://dspace.onu.edu.ua/handle/123456789/19430
dc.language.isoenuk
dc.subjectSarmatian Sea-Lakeuk
dc.subjectBlack Sea region evolutionuk
dc.titleThe processes of the Caspian-Mediterranean corridor formation and the Paratethys Sa-Lake degradationuk
dc.typeArticleuk
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