Stratigraphical position of the Gudå conglomerate zone.

dc.contributor.author	Wolff, Fredrik Chr.
dc.coverage.spatial	SNÅSA
dc.coverage.spatial	VERDAL
dc.coverage.spatial	MERÅKER
dc.date.accessioned	2020-08-26T12:57:42Z
dc.date.available	2020-08-26T12:57:42Z
dc.date.issued	1964
dc.identifier.uri	https://hdl.handle.net/11250/2674795
dc.description.abstract	The 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.iso	eng
dc.relation.ispartofseries	NGU (227)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	PETROGRAFI
dc.subject	PALEOZOIKUM
dc.subject	OMDANNET BERGART
dc.subject	STRATIGRAFI
dc.subject	KALEDONSKE FJELLKJEDE
dc.subject	SEDIMENTÆR BERGART
dc.title	Stratigraphical position of the Gudå conglomerate zone.
dc.type	Journal article
dc.description.localcode	35361
dc.source.pagenumber	85-91 + k

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