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dc.contributor.authorDietrichson, Brynjulf
dc.coverage.spatial17184 Otta
dc.coverage.spatial17183 Skåbu
dc.coverage.spatial17182 Vinstra
dc.coverage.spatial17181 Rondane
dc.coverage.spatialNORD-FRON
dc.coverage.spatialSEL
dc.coverage.spatialVÅGÅ
dc.date.accessioned2020-08-26T12:47:26Z
dc.date.available2020-08-26T12:47:26Z
dc.date.issued1957
dc.identifier.urihttps://hdl.handle.net/11250/2674657
dc.description.abstractThe author sticks to his opposition against Trygve Strand's interpretation (NGU årbok 1955, pp. 43-56) of the metamorphic greenstone with Trondhjemitic veins in Sjodalen as \"gabbro-conglomerate\" of the Valdres Sparagmite sequence. He agrees with professor Strand in emphasizising the importance of the Valdres Sparagmite as a most valuable guideformation in the Caledonides. However, it seems that important facts in V.M. Goldschmidt's (1916A) masterly description of this Caledonian flysch-formation have been disregarded in interpretations of the tectonical chronology of the Caledonides, though the formation occurring between the two Jotum Eruptive Nappes probably provides the most convenient key for solving this fundamental problem. In this respect the author may refer to recently published extensive description of the Caledonides in Southern Swedish Lappland by O. Kulling (1956) who postulates an Eo-Cambrian age for the Valdres Sparagmite (l.c.p. 286) and declares (p. 296) \"the argumentation for Ordovician nappe formations is not valid\". Intending definetely to reject this postulate, and at the same time to give the backround and justify his opposition against Strand's \"gabbro-conglomerate\" of Sjodalen, the author has first summarized some of Goldschmidt's observations and his own investigations.
dc.language.isonor
dc.relation.ispartofseriesNGU (200)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTØRKNINGSBERGART
dc.subjectSPARAGMITT
dc.subjectKONGLOMERAT
dc.subjectPETROGRAFI
dc.subjectSEDIMENTÆR BERGART
dc.subjectGABBRO
dc.titleValdressparagmitten og det såkalte gabbrokonglomerat i Sjodalen.
dc.typeJournal article
dc.description.localcode34998
dc.source.pagenumber8-41


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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