نمایش مختصر رکورد

dc.contributor.authorGoudie, Andrewen_US
dc.contributor.authorKent, P.en_US
dc.contributor.authorViles, H.en_US
dc.date.accessioned1399-07-09T11:00:29Zfa_IR
dc.date.accessioned2020-09-30T11:00:29Z
dc.date.available1399-07-09T11:00:29Zfa_IR
dc.date.available2020-09-30T11:00:29Z
dc.date.issued2016-01-01en_US
dc.date.issued1394-10-11fa_IR
dc.date.submitted2016-08-17en_US
dc.date.submitted1395-05-27fa_IR
dc.identifier.citationGoudie, Andrew, Kent, P., Viles, H.. (2016). Pan morphology, Distribution and formation in Kazakhstan and Neighbouring areas of the Russian federation. Desert, 21(1), 1-13. doi: 10.22059/jdesert.2016.58313en_US
dc.identifier.issn2008-0875
dc.identifier.issn475-2345X
dc.identifier.urihttps://dx.doi.org/10.22059/jdesert.2016.58313
dc.identifier.urihttps://jdesert.ut.ac.ir/article_58313.html
dc.identifier.urihttps://iranjournals.nlai.ir/handle/123456789/393144
dc.description.abstractIn northern Kazakhstan and neighbouring parts of the West Siberian Plain of Russia is one of the world's biggest concentrations of pans. The area has thousands of them. Landsat imagery and Google Earth images indicate their distribution within this semi-arid area and their forms and associated lunette dunes. Many of the pans, most of which are small, wet and shallow, show a characteristic shape and orientation and some have developed in Pleistocene dune fields. Others have developed in old river channels and from the deflation of lake floors. The pans are in a low-relief area developed on Palaeogene, Neogene and Quaternary beds and have been shaped by winds coming from the south west. They occur in an area which is predominantly steppe grassland. Comparisons can be made with other global pan areas in terms of their number, densities, areas, and depths and in terms of the materials on which they have developed, and the climatic conditions that occur here they are found. <br />Highlights <br /> <br />One of the world's biggest, previously unstudied, areas of aeolian pans <br />Data are presented on the main pan morphologies and their morphometry <br />The pans have morphological similarities to those observed in areas like the High Plains of the USA, South Africa, the Pampas of Argentina and Australiaen_US
dc.format.extent1775
dc.format.mimetypeapplication/pdf
dc.languageEnglish
dc.language.isoen_US
dc.publisherUniversity of Tehranen_US
dc.relation.ispartofDeserten_US
dc.relation.isversionofhttps://dx.doi.org/10.22059/jdesert.2016.58313
dc.subjectPansen_US
dc.subjectWind Erosionen_US
dc.subjectKazakhstan steppesen_US
dc.subjectWest Siberian Plainen_US
dc.titlePan morphology, Distribution and formation in Kazakhstan and Neighbouring areas of the Russian federationen_US
dc.typeTexten_US
dc.typeResearch Paperen_US
dc.contributor.departmentOxford University School of Geography and the Environment, South Parks Road, Oxford, OX1 3QY, United Kingdomen_US
dc.contributor.departmentOxford University School of Geography and the Environment, South Parks Road, Oxford, OX1 3QY, United Kingdomen_US
dc.contributor.departmentOxford University School of Geography and the Environment, South Parks Road, Oxford, OX1 3QY, United Kingdomen_US
dc.citation.volume21
dc.citation.issue1
dc.citation.spage1
dc.citation.epage13


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