МОРФОСТРУКТУРА БЕЛОМОРСКОГО РЕГИОНА

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dc.contributor.author Авенариус И.Г.
dc.date.accessioned 2022-05-08T02:20:20Z
dc.date.available 2022-05-08T02:20:20Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=17345339
dc.identifier.citation Геоморфология, 2004, , 3, 48-56
dc.identifier.issn 0435-4281
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/37444
dc.description.abstract The morphostructural subdivision of the White Sea region is based on morphostructural analysis of bathymetric charts, space image interpretation, data on seismicity, recent movements of the earth crust and other geological-geophysical data. Present-day morphostructural pattern of the region has resulted from the vertical and lateral Late Cenozoic differentiated tectonic movements along the complicated system of morpholineaments.
dc.subject Cenozoic
dc.title МОРФОСТРУКТУРА БЕЛОМОРСКОГО РЕГИОНА
dc.type Статья
dc.subject.udc 551.432.8(470.21)
dc.subject.age Cenozoic
dc.subject.age Кайнозой ru


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