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dc.contributor.authorHoltedahl, Olaf
dc.coverage.spatial18162 Eina
dc.coverage.spatial18153 Hønefoss
dc.coverage.spatial18141 Asker
dc.coverage.spatial17132 Porsgrunn
dc.coverage.spatialLIER
dc.coverage.spatialOSLO
dc.coverage.spatialBÆRUM
dc.coverage.spatialASKER
dc.coverage.spatialVESTFOLD
dc.coverage.spatialTELEMARK
dc.coverage.spatialVIKEN
dc.coverage.spatialINNLANDET
dc.coverage.spatialOSLO
dc.coverage.spatialBAMBLE
dc.coverage.spatialPORSGRUNN
dc.coverage.spatialSKIEN
dc.coverage.spatialHOLMESTRAND
dc.coverage.spatialØVRE EIKER
dc.coverage.spatialDRAMMEN
dc.date.accessioned2020-08-26T13:29:20Z
dc.date.available2020-08-26T13:29:20Z
dc.date.issued1912
dc.identifier.urihttps://hdl.handle.net/11250/2675201
dc.description.abstractForkortet: The remarkable development in Norway of several chemico-technical branches of industry during the last twenty to thirty years has immensely increased the use of limestone. The object of the present paper is to contribute to our knowledge of the supply of native limestone. It is confined, however, to the occurrence of limestone in the \"Oslo Field\", indicated on the map, Fig.1, by darker tone. The occurrences in the Oslo Field are all of Ordovician or Silurian Age. As in the case of the palaeozoic sediments, here the lime- stone layers are never horizontal, but, from folding or other causes, are in- clined. The strike in the folded, northern districts is NE-SW to E-W. Descriptions of the several occurrences arranged according to districts menti- oned om pp.12,13 are to be found on pp. 13-63. As the most important occurrences of Ordovician limestone may be mentioned: The Enkrinit-limestone in the Langesund-Skien Valley district, the Gastropod-limestone in the Hadeland, the Mjøs-limestone in the \"Mjøsdistrict\" of Silurian: the Borealis-Pentamerus- limestone in the Hadeland, the Pentamerus-limestone in the Drammen Valley dis- trict, Bærum-Asker-Lier, Ringerike and the Mjøsdistrict, the Wenlock-limestone in the Langesund-Skien Valley district, the limestone of etage 9 d.
dc.language.isonor
dc.relation.ispartofseriesNGU (63)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKARTLEGGING
dc.subjectKALKSTEIN
dc.subjectPETROGRAFI
dc.subjectSEDIMENTÆR BERGART
dc.subjectKJEMISK ANALYSE
dc.titleKalkstensforekomster i Kristianiafeltet
dc.typeJournal article
dc.description.localcode35761
dc.source.pagenumber1-69


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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