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dc.contributor.authorOlesen, Odleiv
dc.contributor.authorEgeland, Bernt
dc.contributor.authorBidstrup, Torben
dc.contributor.authorTorsvik, Trond
dc.contributor.authorBeard, Les
dc.contributor.authorSmethurst, Mark
dc.date.accessioned2020-07-15T08:21:35Z
dc.date.available2020-07-15T08:21:35Z
dc.date.issued1997
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2665856
dc.description.abstractFortrolig til 2002 Potential field data in the Norwegian-Danish Basin have been interpreted. The aeromagnetic anomaly patterns is found to represent three types of magnetic sources: 1) Deep magnetic basement 2) Permian volcanics and intrusives, and 3) Buried sand channels of Quaternary age. The positive gravity effect from the shallow Moho below the Norwegian-Danish Basin is not sufficient to com- pensate for the highly reduced gravity effect from the light sediments within the basin. More dense material has to be introduced at depth in the crust below the deepest part of the westermost Norwegian-Danish Basin and get thin- ner towards the east. The basement depth of the bulk of the Norwegian-Danish Basin varies between 6 and 8 km. Depths between 3 km and 9 km were obtained along the Farsund Basin, and the magnetic anomaly pattern indicates a complex system of fault blocks along the Sorgenfrei-Tornquist Zone.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (97.022)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectMAGNETOMETRI
dc.subjectBERGGRUNNSGEOLOGI
dc.subjectPETROFYSIKK
dc.subjectGRAVIMETRI
dc.subjectTOLKNING
dc.subjectKONTINENTALSOKKEL
dc.titleSAS-96 Part II, Skagerrak Aeromagnetic Survey 1996, Interpretation Report
dc.typeReport
dc.description.localcode44537
dc.source.pagenumber56


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