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Published in 2024 at "Permafrost and Periglacial Processes"
DOI: 10.1002/ppp.2216
Abstract: Multiple parabolic sand dune fields formed in Arctic Sweden after the last deglaciation, facilitated by an abundance of loose glaciofluvial sediment, limited vegetation cover and strong winds. Following initial stabilisation, these dunes underwent repeated reworking…
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Keywords:
dating aeolian;
sweden;
stimulated luminescence;
optically stimulated ... See more keywords