ЭВОЛЮЦИЯ ПРЕДСТАВЛЕНИЙ О ДИНАМИКЕ ЮГО-ВОСТОЧНЫХ БЕРЕГОВ БАЛТИЙСКОГО МОРЯ
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dc.contributor.author | Богданов Н.А. | |
dc.contributor.author | Совершаев В.А. | |
dc.contributor.author | Жиндарев Л.А. | |
dc.contributor.author | Агапов А.П. | |
dc.date.accessioned | 2020-10-12T05:35:05Z | |
dc.date.available | 2020-10-12T05:35:05Z | |
dc.date.issued | 1989 | |
dc.identifier | https://elibrary.ru/item.asp?id=40678684 | |
dc.identifier.citation | Геоморфология, 1989, , 2, 62-69 | |
dc.identifier.issn | 0435-4281 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/18006 | |
dc.description.abstract | The efficient use of the natural resources of coasts essentially depends on how correct are the notions on the long-term evolution of the coastal zone. The concept that the SE Baltic coast evolution is controlled by a single East Baltic debris flow is proved to be inconsistent. A new, non-traditional concept is introduced and substantiated, which considers the Holocene evolution of the SE Baltic coast proceeding by step-by-step development of relatively independent lithodynamic systems. The concept should be taken as a starting point for coast protection measures and rational land use planning in the region. | |
dc.subject | Holocene | en |
dc.title | ЭВОЛЮЦИЯ ПРЕДСТАВЛЕНИЙ О ДИНАМИКЕ ЮГО-ВОСТОЧНЫХ БЕРЕГОВ БАЛТИЙСКОГО МОРЯ | |
dc.type | Статья | |
dc.subject.age | Cenozoic::Quaternary::Holocene | en |
dc.subject.age | Кайнозой::Четвертичная::Голоцен | ru |
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