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dc.contributor.authorHossack, J.R.
dc.coverage.spatial16164 Hemsedal
dc.coverage.spatial16161 Tisleia
dc.coverage.spatial16173 Vangsmjøsi
dc.coverage.spatial16172 Slidre
dc.date.accessioned2020-08-26T13:10:06Z
dc.date.available2020-08-26T13:10:06Z
dc.date.issued1972
dc.identifier.urihttps://hdl.handle.net/11250/2674949
dc.description.abstractEocambrian conglomerates and arkoses were deposited on the Precambrian Jotun rocks. The subsequent polyphase structural evolution of this sequence to form the Grønsennknipa Nappe is described. The emplacement of this nappe over the phyllites of the Quartz Sandstone Nappe to its present position is shown to have occurred during the last movement phase recognized in the area.
dc.language.isoeng
dc.relation.ispartofseriesNGU (281)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectTEKTONIKK
dc.subjectSTRATIGRAFI
dc.subjectKALEDONSKE FJELLKJEDE
dc.subjectKARTLEGGING
dc.subjectPETROGRAFI
dc.subjectSTRUKTURGEOLOGI
dc.titleThe geological history of the Grønsennknipa Nappe, Valdres.
dc.typeJournal article
dc.description.localcode35245
dc.source.pagenumber1-26


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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