ЭВОЛЮЦИЯ СКЛОНОВ ДОЛИН НИЗШИХ ПОРЯДКОВ НА ОСНОВЕ ПРЕДСТАВЛЕНИЙ О ГЕОМОРФОЛОГИЧЕСКОЙ ФАЦИИ (НА ПРИМЕРЕ НИЗКОГОРЬЯ ЮЖНОГО СИХОТЭ-АЛИНЯ)

dc.contributor.author	Невский В.Н.
dc.date.accessioned	2024-03-09T07:07:18Z
dc.date.available	2024-03-09T07:07:18Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=9213569
dc.identifier.citation	Геоморфология, 2006, , 2, 101-109
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/42940
dc.description.abstract	Geomorphologic facie of slopes is specified by two independent parameters: the steepness of the slope and mechanical composition of deposit (or characteristic of denuded slope surface). Using this idea author represents the scheme of mountain relief flattening under the condition of rhythmic fluvial activity. According to idealized scheme the slope evolution is directional discontinuous process, of which every episode includes denudation and accumulative stages. In the reality they may be not strictly separated.
dc.title	ЭВОЛЮЦИЯ СКЛОНОВ ДОЛИН НИЗШИХ ПОРЯДКОВ НА ОСНОВЕ ПРЕДСТАВЛЕНИЙ О ГЕОМОРФОЛОГИЧЕСКОЙ ФАЦИИ (НА ПРИМЕРЕ НИЗКОГОРЬЯ ЮЖНОГО СИХОТЭ-АЛИНЯ)
dc.type	Статья
dc.subject.udc	551.4.037(235.47)

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