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Par Collection Par Auteur- ELVERHOI, A. (1)
- ORHEIM, O. (1)
- 1982 (1)
- depth), with sedimentation rates probably < 0,01 m/ka. The coarse grained texture of these deposits is caused by removal of finer grades in suspension during settling of ice rafted debris sediments. Overconsolidated till was deposited < 31 000 BP during