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dc.contributor.authorMuller, Axel
dc.contributor.authorIhlen, Peter Marcus
dc.contributor.authorSnook, Ben
dc.contributor.authorB. Larsen, Rune
dc.contributor.authorFlem, Belinda
dc.contributor.authorBingen, Bernard
dc.contributor.authorWilliamson, Ben J
dc.date.accessioned2020-05-14T10:16:04Z
dc.date.available2020-05-14T10:16:04Z
dc.date.created2015-11-18T12:17:05Z
dc.date.issued2015
dc.identifier.citationEconomic Geology and The Bulletin of the Society of Economic Geologists. 2015, 110 (7), 1737-1757.en_US
dc.identifier.issn0361-0128
dc.identifier.urihttps://hdl.handle.net/11250/2654422
dc.description.abstractTrace element concentrations in quartz from 188 granitic pegmatites in the Froland and Evje-Iveland pegmatite fields, southern Norway, have been determined to establish exploration targets for high-purity quartz and to gain a better understanding of the genesis of pegmatites hosting these deposits. Both pegmatite fields were formed during the Sveconorwegian (Grenvillian) orogeny (1145–900 Ma) at the western margin of the Fennoscandian Shield.en_US
dc.language.isoengen_US
dc.publisherSociety of Economic Geologistsen_US
dc.titleThe chemistry of quartz in granitic pegmatites of southern Norway: Petrogenetic and economic implicationsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber1737-1757en_US
dc.source.volume110en_US
dc.source.journalEconomic Geology and The Bulletin of the Society of Economic Geologistsen_US
dc.source.issue7en_US
dc.identifier.doi10.2113/econgeo.110.7.1737
dc.identifier.cristin1290372
dc.description.localcodeThis article will not be available due to copyright restrictions (c) 2015 by Society of Economic Geologistsen_US
cristin.unitcode194,64,90,0
cristin.unitnameInstitutt for geovitenskap og petroleum
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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