РЕЛИКТОВЫЙ СУБАЭРАЛЬНЫЙ РЕЛЬЕФ ПОД ВОДАМИ МИРОВОГО ОКЕАНА

dc.contributor.authorЛукьянова С.А.
dc.date.accessioned2021-12-07T03:40:52Z
dc.date.available2021-12-07T03:40:52Z
dc.date.issued2003
dc.description.abstractNumerous examples from various regions (easterm margin of the USA, Puerto-Rico, south-east of Africa, arctic shelf, continental margins of Israel and Bulgaria) illustrate influence of originally subaerial relict landforms of various origin on sediment transport over the shelf. Submerged river valley mostly make obstacles to longshore sediment transport, while relict coastal forms, such as beach ridges and dunes, impede transversal sediment flows.
dc.identifierhttps://www.elibrary.ru/item.asp?id=17349791
dc.identifier.citationГеоморфология, 2003, , 1, 65-72
dc.identifier.issn0435-4281
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/33006
dc.subject.udc551.462:551.4.072
dc.titleРЕЛИКТОВЫЙ СУБАЭРАЛЬНЫЙ РЕЛЬЕФ ПОД ВОДАМИ МИРОВОГО ОКЕАНА
dc.typeСтатья

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