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• W2000570586 abstract "The Weichselian and Holocene sediments in the Lofoten Drift comprise six lithofacies: brown sandy mud, olive grey mud, olive grey laminated mud, dark brown mud, massive sand and dark grey sandy mud. During the Weichselian, the sediment input to the Lofoten Drift was from two main sources, i.e., glacimarine sedimentation and ocean current winnowing. During the Holocene, the sediment input was only from winnowing. The sediment source area was the Vøring margin and the continental margin further south. The sedimentation rate was 190 cm/ka during the late Weichelian and 9 cm/ka during the Holocene. The Weichselian rates are high compared with the deep-sea contourite drifts comprising highly bioturbated sediments, and probably explain why bioturbation is less pronounced in these slope drift sediments. Drifts on glaciated margins, as exemplified by the Lofoten Contourite Drift, represent areas of high sedimentation rate during glacial maxima. Sediment input was not restricted to glacial maximum periods, for sediments also accumulated during other stadial and interstadial periods." @default.
• W2000570586 created "2016-06-24" @default.
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• W2000570586 date "2004-02-01" @default.
• W2000570586 modified "2023-10-04" @default.
• W2000570586 title "Weichselian and Holocene growth of the northern high-latitude Lofoten Contourite Drift on the continental slope of Norway" @default.
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• W2000570586 doi "https://doi.org/10.1016/j.sedgeo.2003.07.004" @default.
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