Blar i NGU Open Archive på emneord "SEDIMENTÆR BERGART"

Viser treff 41-60 av 162

    • Geologiske undersøkelser i den sydøstligste del av Helgeland. 

      Strand, Trygve (NGU (184), Journal article, 1953)
      Helgeland is the southern part of northern Norway. The writerand his assistants have worked in the northern part of the area shownon the map, the southern part of the same map is based upon thegeological maps in manuscript ...

    • Geologiske Undersøkelser i Espedalen. Gradteig Vinstra og tilgrensende høifjell. 

      Dietrichson, Brynjulf (NGU (163), Journal article, 1945)
      This paper deals with a group of mountains situated in Espedalen between Vestre Gauldal and Skabu on the map quadrangle F 30 V, Vinstra. The field work was conducted by the author during the summers 1941-42, and -43. This ...

    • Geologiske undersøkelser ved Kragerø, Holleia og Troms 

      Hofseth, Brit (NGU (157), Journal article, 1942)

    • Geology and structure of the Prestberget area. 

      Strand, Trygve (NGU (228), Journal article, 1964)
      Prestberget er det berg vest for Vågå kirke (med Jutulporten), hvor veien til Nordherad slynger seg oppover. Ved veien ved Bygdetunet er det meget gode blotninger av lagdelte bergarter og det kan her påvises at lagene er ...

    • Geology of the northernmost part of the Meråker area. 

      Siedlecka, Anna; Siedlecki, Stanislaw (NGU (245), Journal article, 1967)
      Four lithostratigraphical groups comprising sedimentary and igneous rocks have been distinguished in the mapped area. There are conformities and gradual transition between all these groups. The rocks have been subjected ...

    • Geology of the western and north-eastern part of the Meråker area. 

      Chaloupsky, Josef; Fediuk, Ferry (NGU (245), Journal article, 1967)
      A thick metasedimentary sequence together with a volcanic and hypabyssal intrusive complex is described. While strata dip generally westwards it can be shown that the succession is, for the most part, inverted; the discovery ...

    • Granite studies II. The Precambrian Flå granite, a geological and geophysical investigation. 

      Smithson, Scott B. (NGU (219), Journal article, 1963)
      The Flå granite is composed of two adjacent elliptical granite bodies, the larger northern Hedal granite and the Ådal granite. The granites are surrounded by banded granodioritic gneisses. Migmatites and augen gneisses are ...

    • Graptolitførende skifere i vestre Gausdal. 

      Bjørlykke, Knut O. (NGU (1), Journal article, 1891)
      Forkortet:The Vestre Gausdal is situated in the central part of Southern Norway, 145 kmnorth of Oslo. It lies on the border-zone between the sparagmite-formation,which is Cambrian, and the overlying Silurian schists, which ...

    • Gravel fraction on the Spitsbergen Bank, NW Barents Shelf. 

      Edwards, Marc B. (NGU (316), Journal article, 1975)
      The gravel fraction of the bottom sediment on the Spitsbergen Bank, located south of Svalbard in the NW Barents Sea, is composed predominantly of clastic sedimentary rocks, especially sandstone and shale. Betwwen sampling ...

    • Grensen fyllitt - Valdres-sparagmitt i strøket sydøst for Grønsennknipa, Vestre Slidre. 

      Holtedahl, Olaf (NGU (213), Journal article, 1961)
      In a paper of 1959 the writer described boundaries between the Ordovician \"phyllite formation\" and the overlying \"Valdres Sparagmite\" in and just east of the Grønsennknipa mountain mass, west of the Valdres valley, and ...

    • Grunnfjellsvinduer i Dividalen, Troms. 

      Gustavson, Magne (NGU (223), Journal article, 1963)
      Two small windows of Precambrian granites were investigated during a few days the summer 1962. Above the granites there follow autochtonous rocks of the Hyolithes Zone, of Lower Cambrian age. On the autochtonous rocks rests ...

    • Håfjellsmulden i Ofoten og dens sedimentære jern-mangan-malmer. Søndre Ofotens malmforekomster II. 

      Foslie, Steinar (NGU (174), Journal article, 1949)
      The sedimentary hematite-magnetite ores of marine origin, occurring within the crystalline mica schists of the caledonian mountain of Northern Norway, belong to a characteristic type of iron ore deposits, internationally ...

    • Hellemobotn og Linnajavrre. Geologisk beskrivelse til kartbladene. 

      Foslie, Steinar (NGU (150), Journal article, 1942)
      The situation of the maps is shown on p. 6. They form the southern continuation of the map Tysfjord, recently described by the author (NGU no. 149). The petrology and chemistry of the rocks are reserved for a special paper. ...

    • Hemsedal og Gol. Beskrivelse til de geologiske gradteigskarter E32V og E32Ø. 

      Bugge, Carl (NGU (153), Journal article, 1939)
      The two accompanying maps cover a territory in the central part of Norway, between Hallingdal and Valdres. The district is built up of Caledonian highland formations and highland eruptives covering the sedimentary formations. ...

    • Hyolithus-sonens basale lag i Vest-Finnmark. 

      Holmsen, Per (NGU (195), Journal article, 1956)
      The basal layers of the \"Hyolithus-zone\" in western Finnmark: The \"Hyolithus- zone\" is a term which has been attached to the autochtonous Cambrian substratum of the Caledonides which can be followed from Laksefjord in ...

    • Høifjeldet mellem Vangsmjøsen og Tisleia (Valdres) 

      Reusch, Hans (NGU (32), Journal article, 1901)
      Forkortet: This region lies in the midst of Southern Norway to the NNW of Oslo. The Valdres valley, shown on the maps, pp.86 and 87 stretches from the Vangsmjøs in the NW the Strandefjord in the SE. The bottom of this ...

    • Høifjeldskvartsens nordøstligste udbredelse 

      Bjørlykke, Knut O. (NGU (14), Journal article, 1894)
      The region treated of in this paper lies to the Northeast of the region described by Reusch in his paper: The region between Bygdin and Bang. Kjerulf has divided the sedimentary strata in central Norway is sparagmite ...

    • I. Fjeldstrøket mellem Lyster og Bøverdalen 

      Rekstad, Johan (NGU (69), Journal article, 1914)
      Forkortet: The tract of land here treated is situated in Southern Norway between Sogne- fjord and Bøverdal, at 61\u00B030'N and at 3\u00B0W of Oslo. The rocks of the region form the following sections: 1. Archaean gneiss ...

    • I. Fra indre Helgeland. Fjeldbygningen og bergartene samt bemerkninger om bergverksdriften 

      Oxaal, John (NGU (59), Journal article, 1911)
      Forkortet: Helgeland, the southern part of the district of Nordland, it situated between about 65\u00B0 and 66 1\/2\u00B0 N. Some of the inner parts of this great district were the object of the author's investigations ...

    • Iagttagelser fra en reise i Finmarken 1890 

      Reusch, Hans (NGU (4), Journal article, 1891)
      Forkortet: In the first part of this paper the author describes the solid rocks, beginning with the East. Near the Russian frontier is the Varanger fiord (map.p.26). From the country south of this fiord only stray observations ...