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    • Kalkstensforekomster i Kristianiafeltet 

      Holtedahl, Olaf (NGU (63), Journal article, 1912)
      Forkortet: 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 ...

    • Kaolin fra Hurdal. 

      Rosenqvist, Ivan Th. (NGU (183), Journal article, 1952)
      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) ...

    • Kaolinforekomst i Hurdalen 

      Homan, C.H. (NGU (1), Journal article, 1891)
      Forkortet: Occurrence of kaolin. Mr. Homan describes a deposit of kaolin resulting from the local decomposition of a syenite in Hurdalen, W of lake Mjøsen.

    • Karasjokgrønnsteinbeltet. Regional geofysisk og geologisk tolkning 

      Midtun, Reidar Devold (Skrifter (88), Book, 1988)
      A geophysical interpretation of geological structures within 5 map-sheets in 1:50,000 scale (AMS M711) has been done. Petrophysical properties of 1350 rock samples and about 11000 in situ susceptibility measurements have ...

    • Karsthuler i Nordland. 

      Horn, Gunnar (NGU (165), Journal article, 1947)
      The cave passages are mostly tunnel shaped, usually with a circular or elliptical section. These passages were formed when they were completely water-filled. Underground streams have later made cuts into the floor of some ...

    • "Kart over Norges malmforekomster" med grafisk fremstilling af "Norges bergverksdrift 1850-97" 

      Vogt, Johan H.L. (NGU (26), Journal article, 1898)

    • Kart-katalog over Norges berggrunn. Catalogue of maps, bed-rock geology of Norway. 

      Dons, Johannes A. (NGU (193), Journal article, 1956)

    • Kartbladet Lillehammer. Tekst 

      Munster, Ths. (NGU (30), Journal article, 1900)
      Forkortet: Diese Abhandlung enthalt eine Beschreibung des geologischen Kartenblattes \"Lillehammer\" (Zwischen 60\u00B0 54' und 61\u00B0 1' N und zwischen ca. 0\u00B0 2' und 0\u00B0 48' west. Lange von Oslo Observatorium). ...

    • Kemiske undersøkelser over ekstration av glimmermineralers kaliindhold. 

      Johnson, E. (NGU (108), Journal article, 1922)

    • Kentallenite (olovine-monzonite) in Bindal, Central Norwegian Caldonides. 

      Nordgulen, Øystein; Mitchell, John G. (NGU Bulletin (413), Journal article, 1988)
      A rock-type identified as kentallenite is reported from the southwestern partof the Helgeland Nappe Complex, Central Norway. The kentallenite is ahypabyssal rock and belongs to a suite of appinitic mafic dykes and smallstocks ...

    • Kisdistriktet Varaldsøy-Ølve i Hardanger og bergverksdriftens historie. 

      Foslie, Steinar; Dietrichson, Brynjulf (NGU (147), Journal article, 1955)
      When Steinar Foslie suddenly passed away in november 1951, he had finished the geological map here presented: \"Kisdistriktet Varaldsøy-Ølve i Hardanger\", based on field-work during 1942-49. Furthermore his M.S. contained ...

    • Kobberforekomster på Straumsheia. 

      Neumann, Henrich (NGU (191), Journal article, 1955)
      The deposits have been known for more than 250 years, and have been worked off and on during that period of time with no great success. The total production has probably not been more than one hundred tons of copper. As ...

    • Komatiitic Chlorite-amphibole rocks and mafic metavolcanics from the Karasjok greenstone belt, Finnmark, northern Norway: a preliminary report. 

      Henriksen, Helge (NGU (382), Journal article, 1983)
      A general account is presented of the field relationships, geochemistry and petrology of mafic and ultramafic metavolcanics within the Precambrian Karasjok greenstone belt. These metavolcanic rocks make up the major part ...

    • Kongsberg Sølvverk. 

      Bugge, Arne (NGU (250 C), Journal article, 1967)
      Kongsberg Silver Mines were worked practically continously from 1623 to 1955. After the Silver Mines were closed down in 1955, all the literature, including the old records and maps, were distributed amongst various ...

    • Kongsberg-Bamble formasjonen 

      Bugge, Arne (NGU (146), Journal article, 1936)
      A prominent friction breccia running from Modum in north to Kristiansund in south divides the pre-Cambrian of Southern Norway into two parts that differ markedly in their geology, petrography, metamorphism and ore deposits. ...

    • Kongsbergfeltets geologi. 

      Bugge, Carl (NGU (82), Journal article, 1917)
      Kongsberg is situated about 80 km west of Oslo at the river Numedalslågen. On p. 8 may be seen a list of the rocks, which occur in the region. All these rocks are of Precambrian age. Besides, there occur dykes of diabase, ...

    • Kongsfjell-områdets geologi, en petrografisk og strukturell undersøkelse i Helgeland, Nord-Norge. 

      Ramberg, Ivar B. (NGU (240), Journal article, 1967)
      The area investigated is situated in the Rødingsfjell nappe of the Norwegian Caledonides in Helgeland, North Norway. The study is divided into two main parts; the first structural and the second petrographic. The first ...

    • Kongsvingerfeltets geologi. 

      Gvein, Øyvind (NGU (246 B), Journal article, 1967)
      The rocks and tectonic features of the Kongsvinger area are described. The area consists of steeply dipping, probably isoclinally folded supracrustal rocks separated by granites, the latter being cataclastic and schistose. ...

    • Kort beretning om Norges Geologiske Undersøkelses ekspedisjon til Birtavarre gruvefelt i Troms, 1952. 

      Gjelsvik, Tore (NGU (184), Journal article, 1953)
      The paper gives a short review of the initial work of a Survey expedition to the southern part of the pyrite ore province of Vaddas-Birtavarre in Northern Norway. The ore bodies occur as concordant bands and lenses in ...

    • Kort beskrivelse av bergartene. 

      Broch, Olaf Anton (NGU Bulletin (155), Journal article, 1940)
      Petrographic inspection of the rocks reveals that all of them, both sedimentary and igneous, are metamorphic. The igneous rocks are gabbroic and trondhjemitic. The rocks of gabbroic origin (among them probably hypabyssal ...