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dc.contributor.authorOftedahl, Christoffer
dc.coverage.spatial17221 Vuku
dc.coverage.spatial15222 Rissa
dc.coverage.spatial15203 Oppdal
dc.coverage.spatial14192 Dombås
dc.coverage.spatialINNLANDET
dc.coverage.spatialOPPDAL
dc.coverage.spatialLESJA
dc.coverage.spatialTRØNDELAG
dc.coverage.spatialSTEINKJER
dc.date.accessioned2020-08-26T12:57:35Z
dc.date.available2020-08-26T12:57:35Z
dc.date.issued1964
dc.identifier.urihttps://hdl.handle.net/11250/2674794
dc.description.abstractThe gneisses below the Cambrian schist or Eocambrian flagstones in the central Norwegian Caledonides have been considered of Precambrian age, but the fact that the contact is always concordant has been explained as due to Caledonian tectonization. The author describes shortly a number of localities of this contact and concludes that a more likely explanation is that the rocks are really close to concordant, e.g. the Precambrian rocks within the Trondheim region were essentially flat-lying at the begin of Cambrian time.
dc.language.isoeng
dc.relation.ispartofseriesNGU (227)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPETROGRAFI
dc.subjectKAMBRIUM
dc.subjectPREKAMBRIUM
dc.subjectPALEOZOIKUM
dc.subjectOMDANNET BERGART
dc.titleThe nature of the basement contact.
dc.typeJournal article
dc.description.localcode35358
dc.source.pagenumber5-12


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