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dc.contributor.authorHoltedahl, H.
dc.contributor.authorBjerkli, Kristian
dc.date.accessioned2020-08-26T13:14:04Z
dc.date.available2020-08-26T13:14:04Z
dc.date.issued1975
dc.identifier.urihttps://hdl.handle.net/11250/2674996
dc.description.abstractThe surface sediments covering the area under consideration can be divided into 4 groups: 1. Till, mainly composed of material derived from the adjacent mainland. 2. Till, mainly containing material derived from Mesozoic-Tertiary bedrock on the continental shelf. 3. Lag deposits from 1 and 2, mainly in shallow areas. 4. Secondarily transported sand and finer material winnowed out from 1 and 2, probably partly mixed with meltwater deposits, and deposited at intermediate and greater depths. There is a clear relationship between depth and sediment texture. The thickness of post-Tertiary sediments varies between 0 and 400 m. In areas with thin cover, the glacial sediments have a lithology greatly influenced by the subsurface rocks.
dc.language.isoeng
dc.relation.ispartofseriesNGU (316)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPLEISTOCEN
dc.subjectSEDIMENTOLOGI
dc.titlePleistocene and recent sediments of the Norwegian Continental Shelf (62°N-71°N), and the Norwegian Channel area.
dc.typeJournal article
dc.description.localcode35886
dc.source.pagenumber241-252


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    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

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