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dc.contributor.authorMalarz, Romanpl_PL
dc.contributor.authorPękala, Kazimierzpl_PL
dc.date.accessioned2019-03-15T10:25:28Z
dc.date.available2019-03-15T10:25:28Z
dc.date.issued1980
dc.identifier.citationRocznik Naukowo-Dydaktyczny. 1980, Z. 71, Prace Geograficzne 8, s. 29-[37]pl_PL
dc.identifier.urihttp://hdl.handle.net/11716/4486
dc.description.abstractDusty forms were found among the Quaternary crusts in the Chentej Mountains in Mongolia. The paper shows their characteristics: an attempt also is made to define the sedimentation conditions of those macroscopically loess-like forms. Their occurrence in the Sugnugurin-gol and Batsumber Valleys was investigated. Three stages of these forms arising were differentiated. Two humid phases wherein weathering-slope crusts had been formed were separated by a dry period with Eolian processes dominating.en_EN
dc.language.isoplpl_PL
dc.titleUtwory pyłowe Kotliny Batsumber i doliny Sugnugurin-gołpl_PL
dc.title.alternativeDusty forms in the Batsumber and Sugnugurin-gol Valleysen_EN
dc.typeArticlepl_PL


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