NGU-publikasjoner: Nye registreringer
Viser treff 641-660 av 7138
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Caledonian structural evolution and tectonostratigraphy in the Rombak - Sjangeli Window and its covering sequences, northern Scandinavian Caledonides
(NGU Bulletin (415), Journal article, 1989)The tectonostratigraphy and Caledonian structural evolution of an area in and around the north-eastern corner of the Rombak-Sjangeli Window (RSW) in the northern Scandinavian Caledonides is described. The investigated area ... -
Isotopic evidence on the age of the Trysil porphyries and granites in eastern Hedmark, Norway.
(NGU (266), Journal article, 1970)Rocks from the (sub-Jotnian) acidic plutonic and volcanic basement complexes in the Trysil area, eastern Hedmark, yield a Rb-Sr isochron age of 1541+-69 million years. This agrees within the limits of error with the isochrom ... -
Strandliniens beliggenhed under stenalderen i det sydøstlige Norge
(NGU (41), Journal article, 1905)Forkortet: Die Lage der Strandlinie w\u00E4hrend der verschieden Abschnitte der postglacialen Hebung. Zur L\u00F6sung dieser Aufgabe wurde eine Revision der fr\u00FCheren Untersuch- ungen \u00FCber die gleichzeitigen ... -
Sea-bed sediments and sediment accumulation rates in the Norwegian part of the Skagerrak
(NGU Bulletin (430), Journal article, 1996)Grain-size analysis show that the sea-bed sediments over large areas in the Norwegian Trench and along its northern slope consist of homogeneous silty clay with a clay content of 50-75% and generally less than 2% sand. ... -
Deglaciation of the continental shelf off southern Troms, North Norway.
(NGU (380), Journal article, 1983)Based on lithostratigraphical and seismic studies, four (possibly five) glacial events are recognized in Andfjorden. The two oldest, the I- and G-events are represented by basal tills. The continental ice sheet probably ... -
High-temperature ultramafic complexes in the North Norwegian Caledonides: I - Regional setting and field relationships.
(NGU Bulletin (405), Journal article, 1986)Forkortet.Four major (25-100 km\u00B2) ultramafic complexes were developed in the Sørøy Nappeduring the second phase of Finnmarkian deformation in the North NorwegianCaledonides. They were emplaced into layered mafic ... -
Oppsprekning, topografi og vannføring i massive dypbergarter. Meddelelser fra Vannboringsarkivet nr. 4.
(NGU (195), Journal article, 1956)Relations between jointing, topography and ground water in massive igneous rocks. In a printed lecture on the hydro-geology of Norwegian rocks (see Nor- wegian text), the author mentions the larvikite and nordmarkite area ... -
Lerfall ved Ness i Harran.
(NGU (166), Journal article, 1946)A very big landslip, the biggest one in our country during the period here dealt with occurred on the beach of the Namsen river. It happened a few hundred m upstreams from the bridge Ness. There were no witnesses to the ... -
Årbok 1953
(NGU (188), Journal article, 1954) -
Om sparagmiten og dens skyvning innen kartbladet Øvre Rendal.
(NGU (161), Journal article, 1943)This paper presents some of the results from the geological mapping of \"Øvre Rendal\". The field work was carried out in the course of 14 weeks, divided on three summers: 1939-1941. Deserving special mentioning for work ... -
Løsmateriale og isavsmeltning i nedre Gudbrandsdalen og Gausdal.
(NGU (228), Journal article, 1964)In the present paper are published some preliminary results of a study on glacigene material in two strongly glaciated valleys in Central Norway, namely Gudbrandsdalen and Gausdal. Particular attention has been paid to ... -
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 ... -
An outline of the geology of the Lyngen peninsula, Troms, Norway. (Abstract)
(NGU (269), Journal article, 1971) -
Structures and ore genesis of the Grimsdalen deposits, southern Trondheim region, Norway.
(NGU (351), Journal article, 1979)The central part of the Grimsdalen area of the southern Trondheim region is occupied by a sequence of metavolcanics with subordinate metasediments, termed the Folla Group, which are correlated with the Støren Group of the ... -
Sulitjelmafeltet. Berggrunnsgeologisk kart - M 1 : 100 000. Beskrivelse.
(Skrifter (93), Map, 1989)The eugeoclinal rocks of the Sulitjelma region occup a large depression in the Norwegian Caldonodrd betwwen the Nasafjell tectonic window of Precambrian rocks in the south and the Tysfjord window in the north. The age of ... -
Age and petrogenesis of the Tinn granite, Telemark, South Norway, and its geochemical relationship to metarhyolite of the Rjukan Group.
(NGU Bulletin (440), Journal article, 2002)The Tinn granite is a Mid Proterozoic, foliated pluton, situated in the central part of the Telemark Sector, South Norway. It is spatially associated with metarhyolite belonging to the Tuddal Formation of the Rjukan Group ... -
Dolomittforekomster ved Kragerø.
(NGU (157), Journal article, 1942) -
Et forøk paa inddeling av det syd-norske grundfjeld
(NGU (95), Journal article, 1922)In the present paper a new subdivision of the precambrian formations of southern Norway is attempted. The older views of the Swedish and Norwegian geologists are first summarised. -
Undersøkelser over norske lerer IV. Norske lerforekomster: B. Møre Sør-Trøndelag, Nord-Trøndelag, delvis Nordland samt resterende del av Akershus, Hedmark og Buskerud fylker.
(NGU (120), Journal article, 1924)The present paper is a sequel to the \"Norwegian Clay Deposits A\". Statens Raa- stofskomites Publikation No. 16 (The State Raw Material Commitee Publication No. 16) by the same author and is chiefly a description of the ... -
Lerras langs Mærradalsbekken nedenfor Ullernchausseen.
(NGU (166), Journal article, 1946)A considerable weight of ballast placed on the slope of the valley beneath Ullern in Aker caused a slide on the 31st of March 1936. A big flake of the clayey ground turned so that its upper part sunk 2-3 m along a 70 m ...