ЭКЗОГЕОДИНАМИЧЕСКИЕ РЕЖИМЫ МОСКОВСКОГО РЕГИОНА

dc.contributor.authorБронгулеев В.В.
dc.contributor.authorЖидков М.П.
dc.contributor.authorМакаренко А.Г.
dc.date.accessioned2021-04-06T02:07:45Z
dc.date.available2021-04-06T02:07:45Z
dc.date.issued2001
dc.description.abstractRecent exogeodynamic regimes in the central part of the Russian Plain – Moscow region – are under consideration. Their distinguishing is fulfilled by K-mean method of cluster analysis; different sets of regimes are determined: from two to six regimes within the region. The quantitative characteristics of the regimes and their spatial distribution are described. Within the accumulation plain the regimes of conservative development are dominant, within the denudation plains the sequence of regimes may be revealed, which correspond to different stages of erosion development of landscape. Exogeodynamic regimes of the Moscow region are strongly influenced by morphostructural differentiation: the amplitudes of neotectonic movements play significant role in their distinction.
dc.identifierhttps://www.elibrary.ru/item.asp?id=21325754
dc.identifier.citationГеоморфология, 2001, , 3, 34-47
dc.identifier.issn0435-4281
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/27526
dc.subjectМОСКОВСКИЙ РЕГИОН
dc.subjectКЛАСТЕРНЫЙ АНАЛИЗ
dc.subjectЭКЗОГЕОДИНАМИЧЕСКИЙ РЕЖИМ
dc.subjectПРОЦЕССЫ И ФАКТОРЫ МОРФОГЕНЕЗА
dc.subject.udc551.4.042(470.311)
dc.titleЭКЗОГЕОДИНАМИЧЕСКИЕ РЕЖИМЫ МОСКОВСКОГО РЕГИОНА
dc.typeСтатья

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