ОСОБЕННОСТИ ФОРМИРОВАНИЯ ВРЕЗАННЫХ ИЗЛУЧИН В ВЕРХНЕМ ТЕЧЕНИИ Р. АМУР

dc.contributor.author	Гусев М.Н.
dc.contributor.author	Ликутов Е.Ю.
dc.date.accessioned	2020-10-26T05:37:35Z
dc.date.available	2020-10-26T05:37:35Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=27378007
dc.identifier.citation	Геоморфология, 1990, , 1, 63-71
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18179
dc.description.abstract	Morphology is discussed of a system of incised meanders developed in the upper reaches of the Amur river (so called Korsakovsky Krivuny). Studies of both meanders and the valley topography at this place indicate a strong influence of tectonic tilted blocks which controls the location, stucture and evolution of the meanders. This influence accounts for the development of all terraces (floodplain included) on one side of the valley within each segment.
dc.title	ОСОБЕННОСТИ ФОРМИРОВАНИЯ ВРЕЗАННЫХ ИЗЛУЧИН В ВЕРХНЕМ ТЕЧЕНИИ Р. АМУР
dc.type	Статья

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