RECENT GEOMORPHOLOGIC REGIMES OF THE EAST EUROPEAN AND WEST SIBERIAN PLAINS: SIMILARITY AND DISSIMILARITY

dc.contributor.author	Bronguleev V.Vad.
dc.contributor.author	Zhidkov M.P.
dc.contributor.author	Makarenko A.G.
dc.date.accessioned	2022-07-18T05:29:13Z
dc.date.available	2022-07-18T05:29:13Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13450086
dc.identifier.citation	Doklady Earth Sciences, 2004, 399, 9, 1275-1279
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38227
dc.description.abstract	The regimes similar for both plains and specific are distinguished as result of cluster analysis applied concurrently for both plains. In particular, for the East-European plain (EE) the intense denudation regimes are characteristic (erosion, karst, slide, complex denudation), whereas for West Siberian plain (WS) - weak denudation and accumulation regimes (thermokarst, bog, weak erosion). For WS regimes distribution zonality is more representative than for EE and WS regimes occupy more compact regions. The observed similarity of three zonal and two regional WS and EE regimes apparently follows from morphoclimatic zonality.
dc.title	RECENT GEOMORPHOLOGIC REGIMES OF THE EAST EUROPEAN AND WEST SIBERIAN PLAINS: SIMILARITY AND DISSIMILARITY
dc.type	Статья

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