НЕКОТОРЫЕ ОСОБЕННОСТИ ОРОГРАФИИ И ГИПСОМЕТРИИ ЗАПАДНОЙ СИБИРИ

dc.contributor.author	Бронгулеев В.В.
dc.contributor.author	Жидков М.П.
dc.contributor.author	Макаренко А.Г.
dc.date.accessioned	2021-12-08T07:10:28Z
dc.date.available	2021-12-08T07:10:28Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=17355771
dc.identifier.citation	Геоморфология, 2003, , 3, 3-9
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/33067
dc.description.abstract	About 6000 height level data of the West Siberian Plain (h max and h min in every cell of 20' x 30') were used in analysis. The northern part the plain has meridional strike of large landforms, its prevailing height level is 55-75 m; the southern part has diagonal strike and prevailing level 95-115 m. The average height of the plain is 96 m - 28 m less than that of the Russian Plain. Height histogram of West Siberia has 2 modes, while the Russian Plain has 4. On the whole relief of West Siberia is closer to graded profile, than that of the Russian Plain, though it is younger than the latter. Positive neotectonic movements being more active and differentiated in the Russian Plain may be the cause for such discrepancy.
dc.title	НЕКОТОРЫЕ ОСОБЕННОСТИ ОРОГРАФИИ И ГИПСОМЕТРИИ ЗАПАДНОЙ СИБИРИ
dc.type	Статья
dc.subject.udc	551.432.8(571.1)

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