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dc.contributor.authorКиселев, В. Н.-
dc.contributor.authorМарзин, И. Г.-
dc.date.accessioned2020-12-07T13:43:11Z-
dc.date.available2020-12-07T13:43:11Z-
dc.date.issued1994-
dc.identifier.citationВестник Белорусского государственного университета. Сер. 2, Химия. Биология. География. – 1994. – № 1. – С. 55-58.ru
dc.identifier.issn0372-5340-
dc.identifier.urihttps://elib.bsu.by/handle/123456789/252142-
dc.description.abstractIn ByeIorussion Polesye in the ice-age the tundra-steppe landscape was characterised by the presence of areas of sand desert with barkhans and other sand formes of relief. The modern dynamics of these formes demands a detailed study with the aim of explaining anthropogenic transformations of the environment of this regionru
dc.language.isoruru
dc.publisherМинск : Университетскоеru
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.subjectЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::Географияru
dc.titleЭоловые формы рельефа Белорусского Полесьяru
dc.typearticleru
dc.rights.licenseCC BY 4.0ru
Appears in Collections:1994, №1 (февраль)

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