Blar i NGU Open Archive på emneord "SEDIMENTÆR BERGART"

Viser treff 21-40 av 162

    • Den kaledonske fjellkjede i Norge. The Caledonian mountain chain in Norway. 

      Bugge, Carl (NGU (189), Journal article, 1954)
      The Caledonian mountain chain in Norway: One of the most important and interesting problems in Scandinavian geology is the structure of the Caledonian Mountain chain, which runs through the country from Hardanger to the ...

    • En nyfunden flek af primordial i Hennungbygden, Grans præstegjeld 

      Andresen, Joh. C. (NGU (1), Journal article, 1891)
      Forkortet: The annexed map shows the locality who is situated about 60 kilometres to the north of Christiania. The alum-shist contains agnostus pisiformis. The overlying mass of the eruptive diabase-porphyrite has probably ...

    • Eocambrian and Lower Paleozoic geology of the Digermul Peninsula, Tanafjord, Finnmark. 

      Reading, H.G. (NGU (234), Journal article, 1965)
      The stratigraphical succession of the Digermul Peninsula consists of about 3000 metres of conformable clastic sediments with carbonates and volcanic rocks absent. It has been divided into two groups. The lower, Vestertana ...

    • Eocambrian rocks on the north-west border of the Trondheim basin. 

      Peacey, J. Springer (NGU (251), Journal article, 1967)
      Three occurrences of Eocambrian rocks on the north and west borders of the Trondhim basin are compared, namely in the Gangåsvatn, Opdal and Tømmerås areas. It is shown that the sequence in the Gangåsvann area consists of ...

    • Et kort tilsvar til dr. J.Kiærs bemærkninger om oversilurien i Brumunddalen 

      Bjørlykke, Knut O. (NGU (37), Journal article, 1904)
      Forkortet: The author replies to Dr.Kiær's remarks. (This yearbook 1904, No.5) on his description of the Upper Silurian in the Brumunddal region (1904, No.2). He points out, that Dr.Kiær has made no new observations, and ...

    • Et langt fremskjøvet "jotundekke" i Rendalen. 

      Holmsen, Per (NGU (184), Journal article, 1953)
      In the central part of the sparagmite district of eastern Norway, three augen- gneiss areas have been known since long ago. T\u00CErnebohm (1896) suggested that the Månkampen area and the Ottlaua area were parts of the ...

    • 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 ...

    • Geochemical inorganic signature of sedimentary rocks in contact with saline water and CO2 

      Sæther, O. M.; Ojala, I. (NGU-Rapport (2010.067), Report, 2011)
      A pilot study was carried out with the intention of establishing a geochemical inorganic signal or \"fingerprint\" of soluble major, minor, and trace elements when different types of reservoir and cap rocks come in contact ...

    • 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, ...