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dc.contributor.authorWolff, Fredrik Chr.
dc.coverage.spatialSNÅSA
dc.coverage.spatialVERDAL
dc.coverage.spatialMERÅKER
dc.date.accessioned2020-08-26T12:57:42Z
dc.date.available2020-08-26T12:57:42Z
dc.date.issued1964
dc.identifier.urihttps://hdl.handle.net/11250/2674795
dc.description.abstractThe Gudå conglomerate zone has been considered to be of Upper Ordovician to Lower Silurian age. The main argument for this conclusion has been that the conglomerates of this zone have been the same pebble composition as some proved Ordovician - Silurian conglomerates. The author describees shortly a number of localities in the Guldå-conglomerate zone, and by comparison with descriptions on localities of conglomerates of known age, he concludes that the former conglomerates are more likely of Lower Ordovician age.
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.subjectPALEOZOIKUM
dc.subjectOMDANNET BERGART
dc.subjectSTRATIGRAFI
dc.subjectKALEDONSKE FJELLKJEDE
dc.subjectSEDIMENTÆR BERGART
dc.titleStratigraphical position of the Gudå conglomerate zone.
dc.typeJournal article
dc.description.localcode35361
dc.source.pagenumber85-91 + k


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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