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dc.contributor.authorSvinndal, Sverre
dc.contributor.authorBarkey, Henri
dc.coverage.spatial14154 Eidfjord
dc.date.accessioned2020-08-26T13:04:04Z
dc.date.available2020-08-26T13:04:04Z
dc.date.issued1967
dc.identifier.urihttps://hdl.handle.net/11250/2674866
dc.description.abstractAn occurrence of breccia, which is thought to have been formed\rby a fluidization process, is described. The breccia is supposed to be\rgenetically related to similar breccias encountered in other parts of\rthe Precambrian of southern Norway. A short comparison is made with the previously described Gardnos breccia.
dc.language.isoeng
dc.relation.ispartofseriesNGU (247)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectBREKSJE
dc.subjectGNEIS
dc.subjectPETROGRAFI
dc.subjectPREKAMBRIUM
dc.subjectTUFF
dc.titleContributions to the geology of Hardangervidda (West Norway) I. An explosion-breccia occurrence in Hjølmodalen.
dc.typeJournal article
dc.description.localcode34896
dc.source.pagenumber44-50


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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