МОРФОСТРУКТУРА БЕЛОМОРСКОГО РЕГИОНА

dc.contributor.authorАвенариус И.Г.
dc.date.accessioned2022-05-08T02:20:20Z
dc.date.available2022-05-08T02:20:20Z
dc.date.issued2004
dc.description.abstractThe 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.identifierhttps://www.elibrary.ru/item.asp?id=17345339
dc.identifier.citationГеоморфология, 2004, , 3, 48-56
dc.identifier.issn0435-4281
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/37444
dc.subjectCenozoic
dc.subject.ageCenozoic
dc.subject.ageКайнозойru
dc.subject.udc551.432.8(470.21)
dc.titleМОРФОСТРУКТУРА БЕЛОМОРСКОГО РЕГИОНА
dc.typeСтатья

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