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Eight depositional facies have been identified in Labrador Slope and Basin cores on the basis of sedimentary structures and textures. These are combined into three genetic groups: (1) hemipelagic facies HI with ice-rafted debris (IRD) and H without IRD (with a combined thickness of about 53% of the total core length); (2) debris-flow facies D (7%) and three turbidite facies (34%) T (thin, fine-grained...
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