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dc.contributor.authorKorneliussen, A.
dc.contributor.authorIhlen, P.
dc.contributor.authorGautneb, H.
dc.contributor.authorFuruhaug, L.
dc.date.accessioned2020-07-15T08:10:47Z
dc.date.available2020-07-15T08:10:47Z
dc.date.issued1999
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2665551
dc.description.abstract(Forkortet) Important rutile deposits in Norway are two of main types: eclogite rutile deposits in Western Norway and metasomatic rutile deposits in the Bamble province of southernmost Norway. Eclogite deposits formed by the metamorphic tranformation of Proterozoic mafic rocks during Caledonian high-pressure metamorphism at 400 Ma. Rutile-bearing eclogites are found in various geologicl sub-provinces from the Bergen region in the south to the Kristiansund region in the north. The metasomatic rutile deposits, such as various rutile-bearing amphibolites and albitites in the Bamble geological province in the southernmost Norway, formed by the metasomatic tranformation of ilmenite-bearing gabbroic and amphibolitic rocks at approx. 1150 Ma.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (99.129 I)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectOMDANNING
dc.subjectRUTIL
dc.subjectEKLOGITT
dc.titleRutile deposits in Norway. Vol. 1: Text.
dc.typeReport
dc.description.localcode49223
dc.source.pagenumber61


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal