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Ice stream configuration and sedimentary processes in Albertini Trough, north of Nordaustlandet, were studied using multibeam bathymetry, seismic reflection and sub-bottom profiles together with sediment gravity cores. Progradational sediment packages in the outer Albertini Trough suggest that streaming ice reached the shelf edge multiple times during the last c. 2.6 Ma. S–N-oriented glacial lineations...
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