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dc.contributor.authorLauritsen, Torleif
dc.contributor.authorMørk, Atle
dc.contributor.authorOlesen, Odleiv
dc.contributor.authorBlomstrand, Lars Berg
dc.date.accessioned2020-07-15T07:47:30Z
dc.date.available2020-07-15T07:47:30Z
dc.date.issued2007
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2664848
dc.description.abstractThis report presents results from 2190 magnetic susceptibility measurements on shallow stratigraphic core from the eastern part of the Norwegian Barents Sea (i.e. Svalis Dome, Nordkapp Basin and Finnmark Platform). The cores represent a total of 1730 metres. The main aims of the project are to characterise and interpret variations in magnetic susceptibility in the Palaeozoic and Mesozoic sedimentary successions offshore eastern Finnmark and to identify the mineralogical source of the magnetism in these sediments. The interval between measurements was originally set to 50 cm. However, some cores were too disintegrated to form a definite and convenient volume.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (2007.028)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectGEOFYSIKK
dc.subjectLABORATORIEMÅLING
dc.subjectLITOLOGI
dc.subjectMAGNETOMETRI
dc.subjectPETROFYSIKK
dc.subjectSTRATIGRAFI
dc.titleOSRAM II - Origin of Sediment-Related AeroMagnetics II. Magnetic susceptibility measurements on shallow stratigraphic cores from the Finnmark Platform, Nordkapp Basin and Svalis Dome
dc.typeReport
dc.description.localcode53038
dc.source.pagenumber105 s.
dc.relation.project(316500) OSRAM II, origin of sediment-related aeromagnetics


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