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dc.contributor.authorWinsborrow, Monica
dc.contributor.authorChand, Shyam
dc.contributor.authorRise, Leif
dc.contributor.authorBøe, Reidulv
dc.date.accessioned2020-07-15T07:30:35Z
dc.date.available2020-07-15T07:30:35Z
dc.date.issued2012
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2664531
dc.description.abstractSandwaves are common on many continental shelves indicating the operation of strong currents which lead to erosion, transportation and deposition of sediment on the seabed. Their dynamic nature means that they can pose challenges to seafloor installations such as pipelines.Sandwaves were identified on the Barents Sea continental margin by the MAREANO programme (www.mareano.no). A project entitled \"Sandwaves and sand transport on the Barents Sea continental margin\", within the Norwegian Deepwater Program, NDP, was set up with the aim to provide a detailed study of the nature and characteristics on sand waves on the Barents Sea continental slope.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (2012.038)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKONTINENTALSOKKEL
dc.subjectMARINGEOLOGI
dc.subjectSEISMIKK
dc.subjectHAVBUNNSTOPOGRAFI
dc.titleCruise report - Sandwaves and sand transport on the Barents Sea continental margin offshore Norway
dc.typeReport
dc.description.localcode60016
dc.source.pagenumber75
dc.relation.project(342000) Sandwaves and sand transport on the Barents Sea continental margin offshore Norway


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal