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dc.contributor.authorBryhni, Inge
dc.contributor.authorJacobsen, Vigdis W.
dc.contributor.authorBrastad, Kjartan
dc.coverage.spatial13161 Gudvangen
dc.coverage.spatial14164 Aurland
dc.date.accessioned2020-08-26T13:23:05Z
dc.date.available2020-08-26T13:23:05Z
dc.date.issued1983
dc.identifier.urihttps://hdl.handle.net/11250/2675153
dc.description.abstractIn the area between Aurlandsfjorden and Nærøyfjorden the Jotun Nappe Complex can be subdivided into a lower thrust unit of mainly gneisses with mangerites, jotunites and minor supracrustals (the Flåm unit), and an upper unit mainly gabbroic to anorthostic rocks (the Stiganosi unit). The basal thrust of the Nappe Complex and the contact between the two internal units are blastomylonitic and characterized by retrogression of the original granulite-facies assemblages. Extensions of investigations into a larger part of the \"Faltungsgraben\" indicates that the tectonic subdivision of the Jotun Nappe Complex into a lower and an upper part has regional significance.
dc.language.isoeng
dc.relation.ispartofseriesNGU (380)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRATIGRAFI
dc.subjectTEKTONIKK
dc.subjectOMDANNET BERGART
dc.subjectKALEDONSKE FJELLKJEDE
dc.subjectPETROGRAFI
dc.subjectSTØRKNINGSBERGART
dc.titleSubdivision of the Jotun Nappe Complex between Aurlandsfjorden and Nærøyfjorden, South Norway.
dc.typeJournal article
dc.description.localcode36175
dc.source.pagenumber23-33


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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