NGU-publikasjoner: Nye registreringer

Viser treff 201-220 av 7138

    • The nature of the basement contact. 

      Oftedahl, Christoffer (NGU (227), Journal article, 1964)
      The gneisses below the Cambrian schist or Eocambrian flagstones in the central Norwegian Caledonides have been considered of Precambrian age, but the fact that the contact is always concordant has been explained as due to ...

    • Geochemistry and palaeogeographical setting of greenstone units on Frosta peninsula, Nord-Trøndelag, Central Norwegian Caledonides 

      Lippard, Stephen J.; Roberts, David (NGU Bulletin (450), Journal article, 2010)
      Volcanic and high-level intrusive rocks of the Støren Nappe exposed on the west coast of Frosta peninsula occur in two, distinct, magmatic units; the bimodal Fånes complex and the metabasaltic Granheim greenstone. North ...

    • Noen observasjoner fra grunnfjellsområdet mellom Randafjorden og svenskegrensen. 

      Hjelle, Audun (NGU (223), Journal article, 1963)
      Precambrian rocks from the area west and east of Mjøsa, South Norway, are described, and modal analyses presented. The main regional divisions are from west to east: Grey plagioclase gneisses, the main granite-mylonite ...

    • Grunnvatnet 

      Rekstad, J. (NGU (92), Journal article, 1922)

    • Oil-leakages on the Øvre Romerike aquifer, Southern Norway 

      Storrø, Gaute; Banks, David (NGU Bulletin (422), Journal article, 1992)
      Two leakages of, respectively 20 m3 and <10 m3 of fuel oil have been investi- gated at Trandum and Sessvollmoen, on Norway's Øvre Romerike aquifer. The hydrocarbon content of the unsaturated and saturated sediments, and ...

    • 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 ...

    • The lead and zinc bearing veins at Tråk in Southern Norway. 

      Røsholt, Bernt (NGU (250 B), Journal article, 1967)
      The nearly vertical zinc and lead bearing veins that cut through Precambrian rocks near the Oslo region at Tråk in Bamle Southern Norway, are described. They can be followed for nearly 2.5 km. A younger introuded diabase ...

    • Tectonostratigraphy in the Velfjord-Tosen region, southwestern part of the Helgeland Nappe Complex, Central Norwegian Caledonides. 

      Løseth, Helge; Thorsnes, Terje (NGU Bulletin (421), Journal article, 1991)
      In the southwestern parts of the Helgeland Nappe Complex, dismembered ophiolites and their cover sequences are imbricated together with nappes consisting dominantly of continentally derived rock units. A local nappe sequence ...

    • Note on gel structures in a pyrite bed, the Grong district. 

      Oftedahl, Christoffer (NGU (205), Journal article, 1959)
      I en kisblokk som ble funnet ved NGU's blokkleting vest for Tunnsjøen i Grongfeltet forekommer det gelstrukturer, se fig. 1 og 2. Slike strukturer anses i alminnelighet å tyde på syngenetisk dannelsesmåte, og de bekrefter ...

    • The Gudbrandsdalen Antiform - a major Late Caledonian structure 

      Sturt, Brian A.; Ramsay, Donald M. (NGU Bulletin (433), Journal article, 1997)

    • New data on net-veined complexes in the Oslo Rift, southeastern Norway. 

      Andersen, Tom; Sørensen, Henning; Morogan, Victoria (NGU Bulletin (442), Journal article, 2004)
      Bodies of basaltic trachyandesite occur in the endocontact zone of the Mykle granite against the large Skrim larvikite massif in the southern part of the Oslo igneous province.\rNew Sr and Nd isotope data indicate that the ...

    • Fra det nordøstlige af Jotunfjeldene 

      Rekstad, Johan (NGU (37), Journal article, 1904)
      Forkortet: This mountain region forms the highest part of Southern Norway between latitudes 61\u00B0 28' and 61\u00B0 46' N. The two highest mountains in Norway, Gald- høpiggen and Glittertinden, lie within the territory. ...

    • Fjeldstrøget mellem Saldalen og Dunderlandsdalen. 

      Rekstad, Johan (NGU (67), Journal article, 1913)
      Forkortet:The region described is situated in the interior of Northern Norway between66\u00B0 30' and 67\u00B0N, and to the east of the Territory treated in The Geology ofNorthern Helgeland, NGU Nr.62.The stratified rocks, ...

    • Norges Geologiske Undersøkelse 

      Reusch, Hans (NGU (70), Journal article, 1914)
      The Geological Survey of Norway. A short account of the history of the Survey.

    • Årbok 1961 

      Bjørlykke, Harald (NGU (215), Journal article, 1962)

    • The structure of Mellene and Heggberg, Valdres. 

      Nickelsen, Richard P. (NGU (243C), Journal article, 1967)
      Structural study of the Valdres Sparagmite and Mellsenn Formation in their type region between the Jotunheim crystalline rocks and the frontal quartzite nappes of the central southern Norwegian Caledonides has revealed ...

    • Vore myrers plantedække og torvarter 

      Holmsen, Gunnar (NGU (99), Journal article, 1923)
      Die vorliegende Abhandlung enth\u00CClt die Resultate einer Untersuchung der Moore Norwegens, ihre Vegetation, sowie ihre Torfarten betreffend. Die Analyse der Vegetation ist nach der Methode von Raunkiær von Hanna ...

    • Rennebu. Fjeldbygningen inden rektangelkartet Rennebus omraade 

      Bugge, Carl (NGU (56), Journal article, 1910)
      Forkortet: The Rennebu sheet embraces an area of about 590 square miles, situated about 28 miles south of Trondheim. Professor Tørnebohm (p.6) and Professor Kjerulf (p.6) have each given their view of the geological ...

    • Nogle optegnelser fra Andøen 

      Reusch, Hans (NGU (36), Journal article, 1902)
      Forkortet: Appendix, by Dr. Reusch. At the Southern border of the coal field one finds, that the Jurassic deposits are separated from the Archæan by faultlines. Studies of the rocks both in the solid parts and in the loose ...

    • Nyttbare sand- og grusforekomster i Syd-Norge. Del I: De geologiske betingelser for deres avsetning. 

      Holmsen, Gunnar (NGU (233), Journal article, 1965)
      The transport and deposition of gravel by glaciers and byglacier-fed streams during the deglaciation, have been principallyresponsible for the types of Quaternary deposits found in our country.This process is described in ...