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dc.contributor.authorVolden, Tore
dc.contributor.authorOttesen, Rolf Tore
dc.contributor.authorBølviken, Bjørn
dc.date.accessioned2020-08-26T09:10:02Z
dc.date.available2020-08-26T09:10:02Z
dc.date.issued1985
dc.identifier.urihttps://hdl.handle.net/11250/2674237
dc.description.abstractForkortet. The geochemistry of the continental crust of the northern part of the Baltic Shield and adjoining Caledonides has been investigated by analysis of till and stream sediment samples collected at a density of sample per c.50 km2. Relative to the average crustal composition, the tills of the northern part of the Baltic Shield are enriched in Ba, Cs, La, Sc U and V and depleted in Cr, Cu, Mg, Mn, Ni and Zn. Several geochemical provinces have been found, of which a belt of high contents of Cr, Mg, Ni and Sc within the Svecokarelian block is prominent. This geochemical structure follows a zone which possibly marks the border between the pre-Karelian basement and the Svecokarelian blocks.
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.subjectGRUS
dc.subjectØKONOMISK GEOLOGI
dc.subjectKVARTÆRGEOLOGI
dc.subjectINGENIØRGEOLOGI
dc.subjectBYGGERÅSTOFF
dc.subjectSAND
dc.titleGeochemical provinces in the northern parts of the Baltic Shield and Caledonides: preliminary results.
dc.typeJournal article
dc.description.localcode34906
dc.source.pagenumber197-207


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