ON THE RELATIONSHIP OF CHANGES IN CASPIAN SEA LEVEL TO NEOTECTONIC MOVEMENTS
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dc.contributor.author | Vdovykin G.P. | |
dc.date.accessioned | 2020-11-02T00:32:31Z | |
dc.date.available | 2020-11-02T00:32:31Z | |
dc.date.issued | 1990 | |
dc.identifier | https://elibrary.ru/item.asp?id=31153504 | |
dc.identifier.citation | Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 1, 85-87 | |
dc.identifier.issn | 0891-5571 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/18369 | |
dc.description.abstract | One of the leading causes of the variations in Caspian Sea level is neotectonic movements, whose pulsational character is determined by solar- (and lunar-) terrestrial relationships. Exogene factors also have their effect - the surface runoff of river waters, the cessation of evaporation of sea water in the Kara-Bogaz-Gol Gulf (since 1980), etc. On the basis of the cyclinal variations in the level of the Caspian Sea that have been discovered, this article proposes a method of graphic prediction of the maximal level of the Caspian Sea to the year 2100. | |
dc.title | ON THE RELATIONSHIP OF CHANGES IN CASPIAN SEA LEVEL TO NEOTECTONIC MOVEMENTS | |
dc.type | Статья |
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