Kaolin fra Hurdal.

dc.contributor.author	Rosenqvist, Ivan Th.
dc.coverage.spatial	19154 Hurdal
dc.date.accessioned	2020-08-26T12:42:24Z
dc.date.available	2020-08-26T12:42:24Z
dc.date.issued	1952
dc.identifier.uri	https://hdl.handle.net/11250/2674602
dc.description.abstract	In 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.iso	nor
dc.relation.ispartofseries	NGU (183)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	LEIR
dc.subject	STØRKNINGSBERGART
dc.subject	PETROGRAFI
dc.subject	KAOLIN
dc.subject	BERGGRUNNSGEOLOGI
dc.subject	OMDANNET BERGART
dc.title	Kaolin fra Hurdal.
dc.type	Journal article
dc.description.localcode	35411
dc.source.pagenumber	5-9

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