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dc.contributor.authorGjelsvik, Tore
dc.coverage.spatialVESTLAND
dc.coverage.spatialMØRE OG ROMSDAL
dc.date.accessioned2020-08-26T12:41:39Z
dc.date.available2020-08-26T12:41:39Z
dc.date.issued1951
dc.identifier.urihttps://hdl.handle.net/11250/2674594
dc.description.abstractThe paper describes the rocks within a large gneiss-area in Sunnmøre district, on the north-west coast of Southern Norway, between Bergen and Trondheim. Besides the dominating granitic gneisses, the rocks consist of remnants of different supracrustal rocks like quartzites, scists, limestones and basaltic lavas. Relatively small bodies of different mafic and ultramafic rocks have been intruded. All the rocks, the supracrustals most thoroughly, have been metamorphosed and replaced (mainly by granitizing agents) in connection with orogenic movements. The author presumably considers the region being a central zone in the Calidonides of Norway.
dc.language.isonor
dc.relation.ispartofseriesNGU (179)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectOMDANNET BERGART
dc.subjectGABBRO
dc.subjectKARTLEGGING
dc.subjectSTØRKNINGSBERGART
dc.subjectSEDIMENTÆR BERGART
dc.subjectPETROGRAFI
dc.titleOversikt over bergartene i Sunnmøre og tilgrensende deler av Nordfjord.
dc.typeJournal article
dc.description.localcode35439
dc.source.pagenumber1-45


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