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dc.contributor.authorFossen, H.
dc.coverage.spatial12163 Stanghelle
dc.coverage.spatial12154 Bruvik
dc.coverage.spatial11151 Bergen
dc.coverage.spatialSAMNANGER
dc.coverage.spatialOSTERØY
dc.coverage.spatialBJØRNAFJORDEN
dc.coverage.spatialBERGEN
dc.date.accessioned2020-08-26T09:11:58Z
dc.date.available2020-08-26T09:11:58Z
dc.date.issued1988
dc.identifier.urihttps://hdl.handle.net/11250/2674262
dc.description.abstractThe Ulriken Gneiss Complex (UGC) and its sedimentary cover, the RundemanenFormation, have been investigated. The UGC is a Precambrian migmatite complexwhich suffered strong but heterogeneous reworking during the Caledonianorogeny. Rocks of the Rundemanen Formation occur along three major shear zonesin the UGC, and although strongly deformed, primary stratigraphic relations arelocally preserved. Based on a few key localities a general stratigraphy hasbeen established. A tentative lithostratigraphic correlation with rocks of theHedmark Supergroup and the Valdres sparagmites of southern Norway may indicatea Late Precambrian age for rocks of the Rundemanen Formation.
dc.language.isoeng
dc.relation.ispartofseriesNGU Bulletin (412)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKONGLOMERAT
dc.subjectKALEDONSKE FJELLKJEDE
dc.subjectPREKAMBRIUM
dc.subjectSTRUKTURGEOLOGI
dc.subjectTEKTONIKK
dc.titleThe Ulriken Gneiss Complex and the Rundemanen Formation: a basement - cover relationship in the Bergen Arcs, West Norway.
dc.typeJournal article
dc.description.localcode35115
dc.source.pagenumber67-86


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