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Kaolin fra Hurdal.

dc.contributor.authorRosenqvist, Ivan Th.
dc.coverage.spatial19154 Hurdal
dc.date.accessioned2020-08-26T12:42:24Z
dc.date.available2020-08-26T12:42:24Z
dc.date.issued1952
dc.identifier.urihttps://hdl.handle.net/11250/2674602
dc.description.abstractIn Hurdal, 60 km NNE of Oslo, there are deposits of a light clay, originating from the decomposition of syenite. Samples from two localities have been investigated and by differential thermal analysis (Diagram fig. 3) proved to consist chiefly of kaolinite. The tables on p. 7 and the histograms fig. 2 give mechanical analyses of the clay.
dc.language.isonor
dc.relation.ispartofseriesNGU (183)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectLEIR
dc.subjectSTØRKNINGSBERGART
dc.subjectPETROGRAFI
dc.subjectKAOLIN
dc.subjectBERGGRUNNSGEOLOGI
dc.subjectOMDANNET BERGART
dc.titleKaolin fra Hurdal.
dc.typeJournal article
dc.description.localcode35411
dc.source.pagenumber5-9


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