ЛОКАЛЬНЫЕ ОСОБЕННОСТИ СОВРЕМЕННЫХ ЭКЗОГЕОДИНАМИЧЕСКИХ РЕЖИМОВ РУССКОЙ РАВНИНЫ

Show simple item record

dc.contributor.author Бронгулеев В.В.
dc.contributor.author Жидков М.П.
dc.contributor.author Макаренко А.Г.
dc.date.accessioned 2021-08-03T04:33:38Z
dc.date.available 2021-08-03T04:33:38Z
dc.date.issued 2002
dc.identifier https://www.elibrary.ru/item.asp?id=23726995
dc.identifier.citation Геоморфология, 2002, , 1, 3-18
dc.identifier.issn 0435-4281
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/30009
dc.description.abstract The paper deals with application of k-means clustering to the analysis of exogeodynamic regimes. Three different regions of Russian Plain were taken for the analysis and the zoning of each one was made on the basis of nine characteristics: precipitation, amount of woodland, amplitude of neotectonic movements, maximal and minimal heights, depth and density of erosion cutting, intensity of landslides and karst processes. Data were obtained by the grid 5'х10'. We consider the area with close mean values of each characteristic, as an area of specific geomorphic regime, the latter defined by the set of values, significantly discrepant from the others. The regions under consideration have different sets of regimes, which nevertheless have some features in common. In every site the regimes of watersheds with low erosion dissection and of deeply dissected slopes are clearly distinguished.
dc.subject ЭКЗОГЕОДИНАМИЧЕСКИЙ РЕЖИМ
dc.subject КЛАСТЕРНЫЙ АНАЛИЗ
dc.subject КОРРЕЛЯЦИОННЫЙ АНАЛИЗ
dc.subject ПРОЦЕССЫ МОРФОГЕНЕЗА
dc.title ЛОКАЛЬНЫЕ ОСОБЕННОСТИ СОВРЕМЕННЫХ ЭКЗОГЕОДИНАМИЧЕСКИХ РЕЖИМОВ РУССКОЙ РАВНИНЫ
dc.type Статья
dc.subject.udc 551.4.042(470.44+470.45+470.53)


Files in this item

Files Size Format View

There are no files associated with this item.

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record