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dc.contributor.authorBryn, Knut Ørn
dc.coverage.spatial20154 Odalen
dc.coverage.spatial20153 Strøm
dc.coverage.spatial20152 Kongsvinger
dc.coverage.spatial20151 Brandval
dc.coverage.spatialKONGSVINGER
dc.coverage.spatialGRUE
dc.coverage.spatialNORD-ODAL
dc.date.accessioned2020-08-26T12:52:58Z
dc.date.available2020-08-26T12:52:58Z
dc.date.issued1962
dc.identifier.urihttps://hdl.handle.net/11250/2674752
dc.description.abstractAn erratic quartizitic boulder, rich in kyanite, was found at Storsjøen, N. Odal, Southern Norway. The boulder also contains lazulite, rutile, pyrite and svanbergite. Lazulite and svanbergite have not been reported from Norway before. The rock is of the same type which has been found at Horrsjøberget, V\u00CCrmland, Sweden, about 80 km E of Storsjøen. The fact that the erratic boulder was found at this locality, indicate that the sedimentary zone at Horrsjøberget continues against north-west and into Norway.
dc.language.isonor
dc.relation.ispartofseriesNGU (215)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectMINERALOGI
dc.subjectSEDIMENTÆR BERGART
dc.subjectKVARTSITT
dc.subjectKVARTÆRGEOLOGI
dc.subjectPETROGRAFI
dc.subjectBLOKK
dc.titleFortsetter Horrsjøbergets sedimentserie inn i Norge?
dc.typeJournal article
dc.description.localcode36103
dc.source.pagenumber5-9


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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