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dc.contributor.authorStrand, Trygve
dc.coverage.spatial17182 Vinstra
dc.coverage.spatialNORD-FRON
dc.coverage.spatialSEL
dc.date.accessioned2020-08-26T13:05:23Z
dc.date.available2020-08-26T13:05:23Z
dc.date.issued1967
dc.identifier.urihttps://hdl.handle.net/11250/2674885
dc.description.abstractA sequence of five separable formations of assumed Eocambrian to Cambrian and earliest Ordovician age are separated by a thrust-plane from the overlying Otta nappe. A lowermost formation of alternating schists and sandstones (often calcareous or dolomitic) and dolomites contains boulder-bearing schists, correlated with Eocambrian glacial horizon of south Norway (Moelv tillite). It is succeeded by a light feldspathic sandstone (\"light sparagmite\") a formation of alternating schists and sandstones (often calcareous or dolomitic), a thick pelitic sequence (phyllites) and an uppermost sandstone. In the eastern part of the area described on the rocks of this sequence are folded on NW-SE axes, two phases of folding have been ascertained, in the western part the structure is largely monoclinal with dips to NW to NNW.
dc.language.isoeng
dc.relation.ispartofseriesNGU (251)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSEDIMENTÆR BERGART
dc.subjectPETROGRAFI
dc.subjectSKIFER
dc.subjectSTRATIGRAFI
dc.subjectKARTLEGGING
dc.subjectSTRUKTURGEOLOGI
dc.titleStratigraphy and structure of eocambrian and younger deposits in a part of the Gudbrandsdal valley district, south Norway.
dc.typeJournal article
dc.description.localcode34937
dc.source.pagenumber93-106


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