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- W1010497597 abstract "This chapter provides an overview of the Quaternary sediments of the North Sea. The base of the Quaternary rarely forms an identifiable seismic marker except adjacent to land, where relatively unconsolidated Pleistocene deposits commonly overstep the Tertiary on to harder pre-Tertiary strata. The distribution of surface sediments up to and including sand-size on the floor of the southern North Sea has been related to the pattern of tidal current velocities. This general relationship undoubtedly exists, and there is clearly a relationship between changes in current velocity and sediment grade. The Norwegian sector to the south of 58° N is approximately triangular in shape, and includes the southern portion of the Norwegian Channel, together with the wide area of shallow banks which surround Great Fisher Bank at a depth of less than 80 m. The southern limit of the sector lies just to the north of Dogger Bank. The various maps of sediment distribution show that the Skagerrak, like the rest of the Norwegian Channel, is floored by mud and other areas of mud occur in the southern and western parts of the sector in local deeps on the flank of Great Fisher Bank." @default.
- W1010497597 created "2016-06-24" @default.
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- W1010497597 date "1979-01-01" @default.
- W1010497597 modified "2023-10-16" @default.
- W1010497597 title "Chapter 7 The Quaternary Sediments of the North Sea" @default.
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- W1010497597 doi "https://doi.org/10.1016/s0422-9894(08)71349-7" @default.
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