Browsing Artikler by Title
Now showing items 987-1006 of 1064
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Torv
(NGU (105), Journal article, 1922)Die grossen Schwierigkeiten in der Versorgung mit Brennmaterialen, unter denen unser Land w\u00CChrend des Weltkrieges zu leiden hatte, brachte auch die Torffrage wieder stark in den Vorgrund. Die Verwendung von Stichtorf ... -
Torvmyrer inden kartbladet "Sarpsborgs" omraade
(NGU (5), Journal article, 1891)The peatmosses studied occur on the eastern side of the Oslofiord in the environs of the small town of Sarpsborg. The first part of the paper contains the description of the individual mosses. The numbers upon the table ... -
Torvmyrernes lagdeling i det sydlige Norges lavland
(NGU (90), Journal article, 1922)Das Pflanzenleben der Moore, das seine Zusammensetzung in erster Reihe der Fuchtigkeit des Bodens verdankt, tr\u00CCgt in Norwegen doch auch stark das Gepr\u00CCge klimatischer Faktoren. Dies tritt deutlich hervor in dem ... -
Trace fossils in the Halkkavarre section of the Dividal Group (?late Precambrian - Lower Cambrian), Finnmark.
(NGU (288), Journal article, 1973)The increasing abundance of trace fossils in the ?late Precambrian to Lower Cambrian sediments of the Dividal Group is comparable with that found in the laterally equivalent but much thicker succession to the east and ... -
Trekk av isbevegelsen og isavsmeltningen i Nordre Gudbrandsdalens fjelltrakter.
(NGU (223), Journal article, 1963)Glacial striae and ice-moulded forms indicate that the earliest direction of glacial flow was towards E, and that the flow at the maximum was towards N or NW. The late-glacial movement, however, seems to have been towards ... -
Trondheim. Beskrivelse til kvartærgeologisk kart 1621 IV - M 1:50 000 (med fargetrykt kart).
(NGU; Skrifter (391; 46), Journal article, 1983)The superficial deposits within the map-sheet Trondheim, Central Norway, are classified and described. The mountains generally have a thin and discontinuous cover of till. In the lowland areas fine-grained marine sediments ... -
Tryktunneller og geologi
(NGU (93), Journal article, 1922) -
"Trysilhevningen". Kambro-ordovicisk stratigrafi i Femundtraktene.
(NGU (215), Journal article, 1962)Diamond drillings carried out 1960 in the vicinity of the lake Femund, near the Swedish border (fig. 1) gave new informations about the cambro-ordovician stratigraphy in the south-eastern miogeosynclinal belt of the ... -
Tundra polygons photographic interpretation and field studies in North-Norwegian polygon areas.
(NGU (223), Journal article, 1963) -
Two sediment cores from the Norwegian Continental Shelf between Haltenbanken and Frøyabanken (64°06`N, 7°39`E)
(NGU (304), Journal article, 1974)Two sediment cores, 1.5 and 4.5 m long, were obtained on the continental shelf west of the coast of Trøndelag, W. Norway, from a depression 320 m deep, and in an area with very thin cover of quaternary deposits. The upper ... -
Tynset. Beskrivelse til det geologiske rektangelkart
(NGU (175), Journal article, 1950) -
Tysfjords geologi. Beskrivelse til det geologiske gradteigskart Tysfjord.
(NGU (149), Journal article, 1941)The situation of the map Tysfjord is shown on p. 10. It comprises a very rugged country between the coast and the frontier, with several glaciers and mountains up to 1744 meter. The present paper contains the geomorphology, ... -
U-Pb age dating and paleotectonic significance of trondhjemite from the type locality in the Central Norwegian Caledonides
(NGU Bulletin (437), Journal article, 2000)Zircon and titanite U-Pb data are reported from the trondhjemite type locality at Follstad, near Støren in Central Norway. A concordant fraction of aricular zircon and an overlapping fraction of titanite give an age of ... -
U-Pb geochronology and geochemistry of trondhjemites and norite pluton from the SW Trondheim Region, Central Norwegian Caledonides
(NGU Bulletin (441), Journal article, 2003)Zircon analyses from two trondhjemites and a biotite norite from a part of the southwestern Trondheim Region have yielded almost identical Early Silurian ages. The biotite norite and one of the trondhjemites, from a quarry ... -
U-Pb zircon age of 469 +- 5 Ma for a metatonalite from the Kjosen Unit of the Lyngen Magmatic Complex, northern Norway
(NGU Bulletin (428), Journal article, 1995)Two fractions of zircon from a tectonised tonalite from within metagabbro of the Kjosen Unit of the Lyngen Magmatic Complex give a concordant U-Pb age of 469 +- 5 Ma. This is interpreted as a minimum age for the Kjosen ... -
U-Pb zircon age of a dolerite dyke from near Hamningberg,Varanger Peninsula, North Norway, and its regional significance
(NGU Bulletin (432), Journal article, 1997)A dolerite dyke cutting very low-grade metasedimentary rocks of the Løkvik- fjellet Group near Hamningberg, NE Varanger Peninsula, Finnmark, has yielded a U-Pb zircon upper intercept age of 567,1 +30\/23 Ma. This ... -
U-Pb zircon age of the Møklevatnet granodiorite, Gjersvik Nappe, Central Norwegian Caledonides
(NGU Bulletin (421), Journal article, 1991)The Møklevatnet granodiorite in the Gjersvik Nappe has yielded a U-Pb zircon age of 456 +- 2MA from three, concordant, mulitigrain fractions. This can also be regarded as a maximum age, Early Middle Caradoc, for the oldest ... -
U-Pb zircon ages of a tonalite and a granodiorite dykefrom the southeastern part of the Bindal Batholith,central Norwegian Caledonides
(NGU Bulletin (446), Journal article, 2006)An elongate tonalite pluton and a c.10 m-thick granodiorite body in the southeastern part of the Bindal Batholithand Helgeland Nappe Complex, Nord-Trøndelag, have yielded U-Pb zircon ages of 429 \u00B12 and 430 \u00B12 Ma, ... -
Undersøgelse af nogle torvprøver
(NGU (14), Journal article, 1894)The samples were collected in Smaalenene and in the district of Romerike to the North-East of Kristiania. The author has studied chiefly the species of mosses. -
Undersøkelser av steinfraksjonens rundingsgrad i glasigene jordarter.
(NGU (266), Journal article, 1970)The main bulk of the stone material in Norway has undergone only one or a few transport phases. A classification has been made for the deposits in the interior of Eastern Norway on the basis of the degree of roundness of ...