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dc.contributor.authorStrand, Trygve
dc.coverage.spatial14204 Stangvik
dc.date.accessioned2020-08-26T12:42:28Z
dc.date.available2020-08-26T12:42:28Z
dc.date.issued1953
dc.identifier.urihttps://hdl.handle.net/11250/2674605
dc.description.abstractThe boundary between the basal gneiss and the overlying micaschists and micaceous gneisses is marked by a thin zone of \"basal quartzite\", but the quartzite is generally not at the exact boundary between the two divisions. Geologic and petrographic observations show an even transition between the two rock types oligoclase-bearing micaschist, oligoclase gneiss and gneiss more or less rich in microcline, the end member of the series being a light massive gneiss of the basal gneiss type. The basal gneiss can thus not belong to a Pre-Cambrian basement complex, its upper part at least must be of Caledonian origin.
dc.language.isoeng
dc.relation.ispartofseriesNGU (184)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPETROGRAFI
dc.subjectOMDANNET BERGART
dc.subjectGNEIS
dc.subjectGRØNNSTEIN
dc.subjectSKIFER
dc.subjectKVARTSITT
dc.titleThe relation between the basal gneiss and the overlying meta-sediments in the Surnadal district, (Caledonides of Southern Norway).
dc.typeJournal article
dc.description.localcode35541
dc.source.pagenumber100-123


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