Browsing Artikler by Title
Now showing items 71-90 of 1064
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Baseflow production from partially peat-covered catchments, Jonsvatnet, Mid-Norway
(NGU Bulletin (422), Journal article, 1992)Forkortet: To their wide areal extent and high water release capability, peatland ecosystems must have a significant, albeit hitherto poorly quantified, influence on baseflow production in partially peatcovered catchments. ... -
Basement Gneiss doming the Uppermost Allochthon in the Bogøy area of Steigen, Nordland, Norway.
(NGU Bulletin (414), Journal article, 1989)Steigen lies geographically within the Uppermost Allochthon, which was emplacedduring the Scandian phase of the Caledonian orogeny. A tectonized boundaryseparates a basement culmination of Precambrian granite-gneisses from ... -
Basement-cover relations and Caledonian tectonostratigraphy of Sandsøya, Grytøya, Åkerøya and Kjøtta, Western Gneiss Region, North Norway.
(NGU Bulletin (431), Journal article, 1996)Rocks of Sandsøya, Grytøya, Åkerøya, and Kjøtta, represent four Caledonian Tectonic settings: (1) pre-Caledonian Baltic crystalline basement of the Western Gneiss Region, including intrusively enclosed supracrustal rocks; ... -
Bavtajohka Interglacial, the oldest Pleistocene vegetational record from Norway
(NGU Bulletin (427), Journal article, 1995)Frie emneord: Paleobotanikk -
Bedrock geology of the Altevatn-Måskanvarri area, Indre Troms, northern Scandinavian Caledonides.
(NGU Bulletin (432), Journal article, 1997)The Altevatn-Måskanvarri area of inner Troms provides a critical link between the more intensively studied areas in northernmost-Sweden and Finnmark to the north. It is composed of a stack of far-travelled Caledonian thrusts ... -
Bemærkningen om endel myrstrækninger i Bergs og Rakkestads præstegjælde i Smaalenenes samt om myrene paa Jæderen
(NGU (1), Journal article, 1891)Forkortet: The peat-mosses studied occur on the eastern side of the Christianafjord in the environs of the small city of Sarpsborg. The upper 2-3 metres of the masses consist of sphagnum, which at the surface is in full ... -
Bemærkninger om oversiluren i Brumunddalen
(NGU (37), Journal article, 1904)Forkortet: The author can not agree in some points of the description of the Upper Silurian in Brumunddalen, which Mr.K.O.Bjørlykke has published in \"Norges geologiske undersøkelses Årbok\" (1904 No.2). I. The graptolitic ... -
Benthic foraminiferal evidence of environmental change in the Skagerrak over the past six decades
(NGU Bulletin (430), Journal article, 1996)High resolution analyses of fossil benthic forminiferal assemblages have been performed on two short (<40cm) sediment cores from the deep Skagerrak Basin, NE North Sea. 210 Pb-datings of replicate cores from the same two ... -
Bergartgange ved Sand i Ryfylke
(NGU (1), Journal article, 1891)Forkortet: Sand is a village on the south-western coast of Norway to the NE of the city of Stavanger. The dykes are dioritic and occur in gneiss. The principal ones are marked on the sketch-map pag. 35 and illustrated in ... -
Bergartsklassifikasjon og kartsammenstilling. Klassifikasjon av bergarter. Rettledning for forfattere av berggrunnskart. Norsk-engelsk og engelsk-norsk ordliste.
(Skrifter (113), Journal article, 1995) -
Beskrivelse av faunaen.
(NGU (155), Journal article, 1940)The fauna here reported from Karmøy is from a light often micaceous calcareous sandstone, the fossils occurring as rusty impressions and casts, mostly deformed and indistinct. Corals and crinoid stems occur in greatest ... -
Beskrivelse til berggrunnsgeologisk kart over strøket Agdenes- Hemnefjord, Sør-Trøndelag.
(NGU; Skrifter (299; 9), Journal article, 1974)The area consists of regional metamorphic gneisses and crystalline schists. Some of the rocks are of Cambrian-Ordovician age, others of Precambrian age. Examples on the former are flagstones (metamorphosed \"sparagmite\") ... -
Beskrivelse til kartbladet Dønna
(NGU (37), Journal article, 1904)Forkortet: This region is situated in the Northern part of the district of Helgeland between 66\u00B0 and 66\u00B0 20' N. A geological map in black is given on pages 4 and 5. The igneous rocks here are granites, gabbro and ... -
Bidrag til Finmarkens geologi
(NGU (84), Journal article, 1918)The present paper is a result of investigations carried out in the most northern district of Norway, during the summers 1914-17, the total amount of time spent in Finnmark being 23 weeks. The studies have been confined to ... -
Bidrag til kundskaben om Nordlands amts geologi
(NGU (4), Journal article, 1891)Forkortet: The author, who has done most of the field work in the greater part of Nordlands amt, for the preparation of the map, gives his observations at length, illustrating them with sections. The landscape p. 168 shows ... -
Bidrag til Skudenessedimentenes geologi
(NGU Bulletin (155), Journal article, 1940) -
Bidrag til Sørlandets kvartærgeologi
(NGU (55), Journal article, 1910)Forkortet: The present paper contains some glaciological observations made in Nedenes amt and Lista og Mandal amt (Sørlandet) in the Southernmost part of Norway. The observations in Lista and Mandal amt have confined to ... -
Big boulders of tillite rock in Porsanger, Northern Norway.
(NGU (247), Journal article, 1967)In 1959 numerous erratic boulders of tillite rock were discovered at the head of Austerbotn, the eastern arm of the Porsangerfjord. Some of the boulders are very big, having volumes of up to 20m3. In 1965 another two ... -
Biotitt-søvitt på Stjernøy, Vest-Finnmark.
(NGU (183), Journal article, 1952)The island of Stjernøy is built up of a complex of gabbroid rocks, which in the valley of Fjellfinndalen (fig. 1) surrounds a body of chiefly calcite-biotite rock more than commonly rich in apatite, clearly of non-sedimentary ... -
Blyglansforekomst på Krækkjeheia, Hardangervidda.
(NGU (200), Journal article, 1957)A lead deposit near Krækkjeheia, Hardangervidda. This short paper presents the main results of an investigation of a galenaspalerite showing on the mountain plateau of Hardangervidda, 160 kms. west of Oslo. The sulfides ...