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Geomorfologiceskie processy v oazisah Antarktidy (na primere oazisa Mak-Merdo). (Processus géomorphologiques dans les oasis du continent antarctique, l'oasis McMurdo servant de référence)
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pediment inclined by 30. General erosion rate (mostly due to deflation) is less than 0,1mm per year, which is lowest for mountain regions. As far as the exogenous processes are concerned, the oases of Transantarctic Mountains are most relevant analogs