European Margin Sediment Dynamics 2003
DOI: 10.1007/978-3-642-55846-7_25
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Sandy Contourites and Pathways of the Norwegian Sea Overflow Water, West of the Faeroe Bank Channel

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(2 citation statements)
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“…Where studied, the areas of the GSR, between Shetland and to Iceland Ridge have revealed a complex pattern of channel pathways controlled by the seabed topography (Dom and Werner, 1993;Kuijpers et al, 1998;Kenyon et al, 2003), bedforms (Masson et al, 2004) as well as sandy, channel-related sediment drifts (Kenyon et al, 2003).…”
Section: Modern Alongslope Processesmentioning
confidence: 99%
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“…Where studied, the areas of the GSR, between Shetland and to Iceland Ridge have revealed a complex pattern of channel pathways controlled by the seabed topography (Dom and Werner, 1993;Kuijpers et al, 1998;Kenyon et al, 2003), bedforms (Masson et al, 2004) as well as sandy, channel-related sediment drifts (Kenyon et al, 2003).…”
Section: Modern Alongslope Processesmentioning
confidence: 99%
“…The circulation was modified from Hansen and Østerhus (2000); Orvik and Niiler (2002), and Isachsen (2003). SCZarea of sandy contourites (Kenyon et al, 2003). Location of Figs.…”
Section: Oceanographymentioning
confidence: 99%