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dc.contributor.authorOften, M.
dc.contributor.authorElvebakk, G.
dc.contributor.authorKrill, A. G.
dc.date.accessioned2020-08-26T09:10:47Z
dc.date.available2020-08-26T09:10:47Z
dc.date.issued1985
dc.identifier.urihttps://hdl.handle.net/11250/2674248
dc.description.abstractA remarkably little-deformed sandstone in a roadcut near Karasjok showssedimentary structures characteristic of a subaerially exposed tidalenvironment. The fining upward sequence displays flaser bedding, parallellamination, mudclasts, bimodal cross bedding, and mudstone layers withshrinkage cracks. The sandstone is stratigraphically in about the centerof the Karasjok Greenstone Belt, and indicates a shallow-marine environmentfor at least some of the deposits.
dc.language.isoeng
dc.relation.ispartofseriesNGU Bulletin (403)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSANDSTEIN
dc.subjectPREKAMBRIUM
dc.subjectSEDIMENTOLOGI
dc.titleEarly Proterozoic shallow-marine albite-rich sandstone in the Karasjok Greenstone Belt, Norway.
dc.typeJournal article
dc.description.localcode36124
dc.source.pagenumber113-118


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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