Lateglacial river sediment budgets in th
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Huisink, Margriet
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Article
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1999
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John Wiley and Sons
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English
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Three Weichselian Lateglacial (13ยฑ10 ka) terraces have been distinguished in the Maas valley which were formed when the Maas repeatedly incised in an increasingly narrow floodplain. The River Maas changed from a braided system (before c. 12ยด5 ka) via a transitional phase to a high-sinuosity meanderi