ГЕОМОРФОЛОГИЧЕСКИЙ ОЧЕРК ЮЖНОГО МАКРОСКЛОНА СТАНОВОГО ХРЕБТА

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dc.contributor.author Ликутов Е.Ю.
dc.date.accessioned 2021-12-08T07:10:31Z
dc.date.available 2021-12-08T07:10:31Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=17360971
dc.identifier.citation Геоморфология, 2003, , 4, 72-87
dc.identifier.issn 0435-4281
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/33099
dc.description.abstract Special geomorphologic investigations were carried out at the southern slope of Stanovoi ridge. Slopes are shown to play the main role in the tructure and zoning of landforms; the stable slope associations of different dynamic types, an important role of tectonic tilts of land surface, self-development capability are the main features of the relief.
dc.title ГЕОМОРФОЛОГИЧЕСКИЙ ОЧЕРК ЮЖНОГО МАКРОСКЛОНА СТАНОВОГО ХРЕБТА
dc.type Статья
dc.subject.udc 551.4.035(235.34)


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