Now showing items 21-40 of 62

    • Foraminifera in late quaternary deposits from the Oslofjord area. 

      Feyling-Hanssen, Rolf W. (NGU (225), Journal article, 1964)
      Approximately 2500 core samples from 130 borings, 4 m to 40 m deep, in Late Quaternary (latest Allerød through Sub-Atlantic) clay deposits in the Oslofjord area in southeastern Norway were investigated micropaleontologically. ...
    • Foraminiferfaunaen i en del sedimentkjerner fra indre Oslofjord. 

      Risdal, Dag (NGU (224), Journal article, 1963)
      Undersøkelsen er basert på 13 korte sedimentkjerner tatt på forskjellige lokaliteter og dyp i indre del av Oslofjorden. Målet har vært å studere og sammenligne den historiske utvikling av foraminferfaunaen, samt den arts- ...
    • Foraminiferfaunaens relasjon til dybdeforholdene i Oslofjorden, med en diskusjon av de senkvartære foraminifersoner. 

      Risdal, Dag (NGU (226), Journal article, 1964)
      Hovedvekten i arbeidet er lagt på et bathygrafisk studium av foraminiferfaunaen i Oslofjorden, ved at det er tatt prøver i en del profiler i forskjellige deler av fjorden - fra grunt til dypt vann. Foraminiferfaunaene i ...
    • Foreløbige meddelelser fra reiser i Mjøsegnene, udførte for den geologiske undersøgelse sommeren 1889 

      Münster, Ths. (NGU (1), Journal article, 1891)
      Forkortet: The sheet of our maps, named Lillehammer, sketched on pag. 18 is the southern continuation of the sheet \"Gausdal\" surveyed by Mr. Bjørlykke (at the southernmost border together with the present author). From ...
    • Fossiler fra Smølen 

      Holtedahl, Olaf (NGU (69), Journal article, 1915)
      Forkortet: In the following the author describes a few fossils from a limestone of a some- what crystalline character from the island of Smøla. Fossils are very rarely found in this part of Norway, on account of the ...
    • Fossils from pebbles in the Biskopåsen Formation in Southern Norway. 

      Spjeldnæs, Nils (NGU (251), Journal article, 1967)
      Fossils are reported from pebbles in the lowest part of the Biskopåsen Conglomerate in the Late Precambrian Lillehammer Subgroup at the norhtern end of lake Mjøsa in Southern Norway. The most common and widespread fossils ...
    • 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 ...
    • Jæderens geologi. 

      Bjørlykke, Knut O. (NGU (48), Journal article, 1908)
      Forkortet:Jæren is the comparatively flat district on the South Western coast of Norway,between Stavanger and Egersund. The soil consists in most parts, of deposits ofloose material, moraine sand and gravel, peat moss and ...
    • 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 ...
    • Kulforekomsten paa Andøen 

      Dahll, Tellef (NGU (4), Journal article, 1891)
      Forkortet: A map and section are given p. 132. \"Myr\" signifies peatmoss, \"sandsten\" sand- stone, \"lerjernsten\" clay ironstone, \"bitumines skifer\" bituminous shale, \"skjælmergel\" shell-marl, \"borhul\" borehole, ...
    • Lower and Middle Cambrian trilobits from the Digermul peninsula, Finnmark, northern Norway 

      Nikolaisen, Frank; Hemmingsmoen, Gunnar (NGU Bulletin (419), Journal article, 1990)
      Ten trilobite species are described. The only Lower Cambrian one is the olenellid Kjerulfia lata from the upper member (D2) of the Doulbasgaissa Formation, previously known from southern Norway. The Middle Cambrian species ...
    • Marine kvartær-fossiler fra Seimsjøen i Sør-Odal. 

      Feyling-Hanssen, Rolf W. (NGU (205), Journal article, 1959)
      The locality is situated 67 km NE of Oslo centre, at the outlet of Seimsjøen, the southwestern extension of Storsjøen lake (water level 130 m above sea level). Borings were undertaken by the Norwegian Geotechnical Institute, ...
    • Microfossils from late Precambrian sediments around lake Mjøsa, Southern Norway. 

      Manum, Svein (NGU (251), Journal article, 1967)
      Microfossils extracted with ordinary palynological methods from the Biskopås conglomerate (Biri-conglomerate) and the Biri-shale of the late Precambrian age in Southern Norway are described. Two principle categories of ...
    • Micropaleontology applied to soil mechanics in Norway. Mikropaleontologi anvendt på geotekniske problemer i Norge. 

      Feyling-Hanssen, R.W. (NGU (197), Journal article, 1957)
      A breif review of the geological history of the Late Pleistocene marine clay deposits of the Oslofjord area, southeastern part of Norway, has been given, and a stratigraphical division of these sediments, established upon ...
    • Mikropaleontologiens teknikk. 

      Feyling-Hanssen, Rolf W. (NGU (203), Journal article, 1958)
      Technique of micropaleontology: The article describes the treatment of Formanifera samples from Norwegian Late Pleistocene marine clays. The samples is collected with a thin-wall, stationary piston samper with entrance ...
    • Moraines in the Hemnefjord area, Western Norway. 

      Lasca, N.P. (NGU (266), Journal article, 1970)
      Four radiocarbon dates are used to date moraines in the inner Hemnefjord area. The radiometric ages of moraines range from approximately 10,720 to 11,310 years B.P. and probably correlate with the Ra moraines in Southern ...
    • Neotectonic studies in the Ranafjorden area, northern Norway. 

      Olesen, Odleiv; Skogseth, Terje; Olsen, Lars; Karlsen, Tor Arne; Henkel, Herbert; Gjelle, Svein (NGU-Rapport (94.073), Report, 1994)
      The Ranafjorden area in northern Norway is a region of increased seismicity andanomalous land uplift. There is evidence for recent movements in the bedrock;1) A total of 0.89 m uplift of a bladder wrack mark from 1894 to ...
    • New data on Upper Ordovician conodonts from theTrondheim Region, Central Norwegian Caledonides 

      Tolmacheva, T. Ju; Roberts, David (NGU Bulletin (447), Journal article, 2007)
      A small collection of Upper Ordovician (Early-Mid Katian) conodonts has been recovered from low-grade meta-limestones in the K\u00F6li Nappes of the Upper Allochthon of the Trondheim Region, central Norway. For the Snåsavatnet ...
    • New fossil finds from the Cambro-Silurian meta-sediments on Hardangervidda. 

      Andresen, Arild (NGU (304), Journal article, 1974)
      The occurrence of Actinoceroid cephalopods (Ormoceras(?) sp.), brachipods (Orthis ss.), and trilobites (Ptychopyge sp.) in a crystalline limestone overlying bluish quartizite on Hardangervidda indicates that Orthoceras ...
    • Norges kvartærgeologi. En oversigt. 

      Bjørlykke, K.O. (NGU (65), Journal article, 1913)
      Forkortet:The first part contains an historical survey of the works of the Norwegianquaternary geologists in somewhat chronological order, commencing withJens Esmark (1763-1839), who as early as 1824 described the first ...