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- W2115096304 abstract "Abstract The Lofoten Contourite Drift is located below c . 1000 m water depth on the continental slope off northern Norway. It has a maximum thickness of about 360 m and correlation to published seismic stratigraphy implies a Neogene age. The drift probably originated from the deposition of suspended sediments derived from winnowing of the shelf and upper slope. The geometry of the uppermost part of the drift is characterised by maximum thickness at the mound crest, which implies that it is probably presently active. Within gravity core JM97-950/1 (1160 m water depth), the upper 86 cm represents sediments resulting from Holocene winnowing of the shelf and upper slope. The underlying sediments, to 5.5 m core depth, were deposited in a late Weichselian glacimarine environment as revealed by its content of ice-rafted debris and the dating results. Late Weichselian drift growth is consistent with a circulation system transporting surface water northeastward along the continental margin of Norway also during the Weichselian. The downslope sediment input to the study area was probably relatively low during glacial periods due to the evolution of the nearby mainland area, the Lofoten Islands. These islands may have acted as a sediment barrier causing large fluvial and/or glacial drainage systems from central Fennoscandia to be routed south and north of the study area. As a result, alongslope sediment transport has provided the main sediment input to this part of the continental slope." @default.
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- W2115096304 date "2002-01-01" @default.
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- W2115096304 title "The Lofoten Drift, Norwegian Sea" @default.
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- W2115096304 doi "https://doi.org/10.1144/gsl.mem.2002.022.01.05" @default.
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