Browsing Artikler by Subject "SEDIMENTÆR BERGART"

Now showing items 21-40 of 148

    • Ett fossilfynd i Susendalen. 

      Kautsky, Gunnar (NGU (184), Journal article, 1953)
      Ein Fossilfund in den Randteilen des m\u00CCchtigen Kalkmarmors im Susental wird als Rest einer Kalkalge gedeutet (fig. 1). Das Gestein ist stark umkristallisiert. F\u00FCnf D\u00FCnnschlife nach verschiedenen Ebenen durch ...

    • 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 ...

    • Foreløpige meddelelser fra kartbladet Essandsjø. 

      Bjørlykke, Unni (NGU (223), Journal article, 1963)
      A symposis is given of 4-5 weeks of field work in the Sylene area, Sør-Trøndelag, Norway, in the eastern part of the Cambro-Silurian geosyncline of Trondhjemsfeltet. Previous investigations are reffered to. The rocks in ...

    • Fortsetter Horrsjøbergets sedimentserie inn i Norge? 

      Bryn, Knut Ørn (NGU (215), Journal article, 1962)
      An erratic quartizitic boulder, rich in kyanite, was found at Storsjøen, N. Odal, Southern Norway. The boulder also contains lazulite, rutile, pyrite and svanbergite. Lazulite and svanbergite have not been reported 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 ...

    • Fossilførende sedimenter ved Skudenes. 

      Isachsen, Fridtjov (NGU (155), Journal article, 1940)
      The southern part of the island Karmøy (Western Norway, between Stavanger and Haugesund) displays a varying complex of slightly metamorphic sediments and igneous rocks: besides gabbro, there occur conglomerates, \"fragmental ...

    • 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 ...

    • 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. ...

    • Fra Hardangervidden I 

      Reusch, Hans (NGU (34), Journal article, 1902)
      Forkortet: The map on p.29 shows the chief geological divisions. Brøgger has found that the succession of strata in the Hårteigen Mountain has been as follows. 1. Lowermost, lying on old granite, Alum-schist (in Hulberget ...

    • Fra Hardangervidden III 

      Bjørlykke, Knut O. (NGU (34), Journal article, 1902)
      Forkortet: The border-lines on the southwestern and southern part of the map on p.29 are to be attributed to Mr.Bjørlykke, who had a very wild region to explore. His photo, reproduced on p.63, shows veins of granite in ...

    • Gabbrokonglomeratet i Sjodalen. 

      Strand, Trygve (NGU (195), Journal article, 1956)
      The Gabbor Conglomerate in Sjodalen. The area dealt with in the present paper is a part of the valley of the river Sjoa (Sjodalen) in central southern Norway, about 61o42'N and 9o18'E. An account of the general geology of ...

    • Geological and petrographical investigations in the Kongsberg-Bamble formation. 

      Bugge, Jens A.W. (NGU (160), Journal article, 1943)
      The rocks of the Kongsberg-Bamble Formation are Pre-Cambrian and belong to the deeper parts of an ancient mountain range (the Sveco-Fennides). The main geological features appear from Table 11. In comparison with the ...

    • Geological investigation of a lower tertiary/quaternary core, offshore Trøndelag, Norway. 

      Bugge, T.; Maisey, G.H.; Rokoengen, K.; Skaar, F.E.; Thusu, B.; Løfaldli, M. (NGU (316), Journal article, 1975)
      Seismic profiling carried out offshore Trøndelag, Norway, has provided a basis for selecting localities for core sampling of the bedrock. A continous, metre-long core revealing new information was recorded. Sedimentological, ...

    • 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 ...