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dc.contributor.authorPeacey, J. Springer
dc.coverage.spatial17221 Vuku
dc.coverage.spatial17233 Steinkjer
dc.coverage.spatial17232 Snåsavatnet
dc.coverage.spatial18233 Snåsa
dc.coverage.spatialTRØNDELAG
dc.coverage.spatialVERDAL
dc.coverage.spatialSTEINKJER
dc.coverage.spatialMØRE OG ROMSDAL
dc.coverage.spatialSNÅSA
dc.date.accessioned2020-08-26T13:05:09Z
dc.date.available2020-08-26T13:05:09Z
dc.date.issued1967
dc.identifier.urihttps://hdl.handle.net/11250/2674882
dc.description.abstractThree occurrences of Eocambrian rocks on the north and west borders of the Trondhim basin are compared, namely in the Gangåsvatn, Opdal and Tømmerås areas. It is shown that the sequence in the Gangåsvann area consists of two parts: a lower, highfolded succession which, in geological setting, resembles the Opdal area and an upper, lower-grade unit which closely compares with the succession in the Tømmerås anticline. The two are separated by a major tectonic break which marks the border of the \"Trondheim region\" proper.
dc.language.isoeng
dc.relation.ispartofseriesNGU (251)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSANDSTEIN
dc.subjectSEDIMENTÆR BERGART
dc.subjectKVARTSITT
dc.subjectPETROGRAFI
dc.subjectPREKAMBRIUM
dc.subjectOMDANNET BERGART
dc.titleEocambrian rocks on the north-west border of the Trondheim basin.
dc.typeJournal article
dc.description.localcode34936
dc.source.pagenumber83-92


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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