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Changing fluvial style of periglacial lowland rivers during the Weichselian Pleniglacial in the eastern Netherlands in Periglacial processes and landforms.
(supprimer)
Analysis of the fluvial deposits occurring in the Weichselian basin fills in the Twente region contributes valuable information to the interpretation of last Glacial paleoenvironments. Although quantification of paleohydrologic data is difficult