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dc.contributor.authorSundvor, Eirik
dc.date.accessioned2020-08-26T13:14:48Z
dc.date.available2020-08-26T13:14:48Z
dc.date.issued1975
dc.identifier.urihttps://hdl.handle.net/11250/2675017
dc.description.abstractThe southern Barents Sea is underlain by sediments of varying thickness and physical properties. The thick sequence of Tertiary sedimentary rocks, which is representative of the southern provinces of the Norwegian continental margin, is found only as a wedge near the shelf edge of the Barents Sea. Structures that can be associated with salt diapirs are recorded in a limited area on Tromsøflaket.
dc.language.isoeng
dc.relation.ispartofseriesNGU (316)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSEDIMENTÆR BERGART
dc.subjectSEDIMENTOLOGI
dc.titleThickness and distribution of sedimentary rocks in the southern Barents Sea.
dc.typeJournal article
dc.description.localcode35908
dc.source.pagenumber237-240


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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