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dc.contributor.authorNaterstad, Johan
dc.contributor.authorJorde, Knut
dc.contributor.authorAndresen, Arild
dc.coverage.spatialVINJE
dc.coverage.spatialULLENSVANG
dc.coverage.spatialTELEMARK
dc.coverage.spatialVESTLAND
dc.coverage.spatial14144 Haukelisæter
dc.coverage.spatial13141 Røldal
dc.date.accessioned2020-08-26T13:10:55Z
dc.date.available2020-08-26T13:10:55Z
dc.date.issued1973
dc.identifier.urihttps://hdl.handle.net/11250/2674961
dc.description.abstractIt is concluded from reconnaissance studies on Hardangervidda that a succession of 5 allochthonous units occurs above the Precambrian basement and its autochthonous\/parautochthonous cover. The units are named from bottom to top: Holmsjø Formation, Dyrskard Group, Nupsfonn Complex, Kvitenut Complex and Revsegg Formation. Metamorphism in granulite facies (Kvitenut Complex) and subsequent amphibolite facies (upper 4 units) took place outside the present area. Movement between the units occurred in the Precambrian as well as during late Caledonian tectonic phases.
dc.language.isoeng
dc.relation.ispartofseriesNGU (292)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRUKTURGEOLOGI
dc.subjectKARTLEGGING
dc.subjectTEKTONIKK
dc.subjectKALEDONSKE FJELLKJEDE
dc.subjectPETROGRAFI
dc.subjectSTRATIGRAFI
dc.titleTectonic succession of the Caledonian nappe front in the Haukelisæter- Røldal area, Southwest Norway.
dc.typeJournal article
dc.description.localcode36291
dc.source.pagenumber1-20 + ka


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