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Sunndalsøra 1420 III. Beskrivelse til kvartærgeologisk kart - M 1 : 50 000 (med fargetrykt kart).
(Skrifter (79), Map, 1987)The superficial deposits within the map-sheet are described and genetically classified. Tills are the dominating sediments, but considerable amounts of glaciofluvial and fluvial deposits also occur. Slide and talus deposits ... -
Supergene alteration of Norwegian Sulphide deposits - a query.
(NGU (213), Journal article, 1961)Forfatteren diskuterer en tidligere avhandling av Bjørlykke som behandler spørsmålet om supergene anrikninger i norske kisforekomster. Bjørlykkes forslag er at anrikninger av kobber, utelukkende som kobberkis (kalkopyrit), ... -
Supergene anrikninger av kopper i våre kisforekomster
(NGU (211), Journal article, 1960)The Norwegian copper-bearing pyrite deposits generally show a higher content of copper near the surface than the average content of the whole ore body. This may be due to a secondary supergene sulphide enrichment caused ... -
Supracrustal and infracrustal rocks in the Gneiss region of the Caledonides west of Breimsvatn.
(NGU (266), Journal article, 1970)Two rock complexes can be distinguished in the Gneiss region west of Breimsvatn in Sogn & Fjordane, West Norway. The upper complex is composed essentially of original supracrustal rocks: calcareous, psammitic and pelitic ... -
Suspension sedimentation of coarse silt and sand in northern Skagerrak: textural and mineralogical trends
(NGU Bulletin (430), Journal article, 1996)The minor coarse-silt and sand fraction of muddy bottom sediments at 74 sites in northern Skagerrak is interpreted to have been mostly transported in suspension, aided by frequent reworking and the buoyancy of large ... -
Svekokarelian thrusting with thermal inversion in the Karasjok-Levajok area of the northern Baltic Shield
(NGU Bulletin (403), Journal article, 1985)Recent mapping, isotopic dating, and metamorphic and structural observations from the Karasjok-Levajok are, lead to a tectonic interpretation that is similar in many ways to Phanerozoic plate tectonic models. Three major ... -
Syd-Norges gruber og malmforekomster.
(NGU (126), Journal article, 1925)On the map accompanying this paper all the mines and ore deposits of Southern Norway are collected for the first time.The material has been gathered from printed and unprinted sources, communications from mining engineers ... -
Sydøstligste Helgelands geologi.
(NGU (191), Journal article, 1955)Geology of the south-eastermost part of Helgeland: Helgeland is the southern part of northern Norway. The present paper is a preliminary report presenting the results of mapping work during the summers 1951-54 by the writer ... -
Søndre Femund. Beskrivelse til det geologiske rektangelkart.
(NGU (148), Journal article, 1937)This map covers the area between the Swedish border to the east, the foot of the mountains Rendalssølen and Gloføken to the west. The predominant part of the surface is covered up by glacial drift of great thickness and ... -
Søndre Helgeland, Svenningdalens sølvertsgange (I Vefsen, søndre del af Nordlands amt).
(NGU (29), Journal article, 1900)Forkortet:In Svenningsdalen in Grane, ca. 44 Km sudlich von der kleinen Hafenstadt Mosjøen, ist ein ca. l km langes Erzfeld, das 15-20 grøssere und mehrere kleinere Erzgange (s.Tafel 1) umfasst, die seit 1877 bergmannisch ... -
Sørlandet i sen- og postglacial tid.
(NGU (210), Journal article, 1960) -
Talk-serpentinforekomster i Sparbu, Nord-Trøndelag.
(NGU; Skrifter (290; 4), Journal article, 1973)The report presents a technical description of certain talc-serpentine deposits occuring within the Gula Schist Group (Cambrian) of the Trondheim region. No form of contact metamorphism of the schist can be observed along ... -
Tectonic evolution of the Northeast Atlantic ocean: a review.
(NGU (316), Journal article, 1975)The hypotheses of sea floor spreading and plate tectonics enable the evolution of ocean basins to be understood provided that there are adequate data on the present and past plate boundaries from the magnetic anomaly ... -
Tectonic features of an area N.E. of Hegra, Nord-Trøndelag, and their regional significance - preliminary notes.
(NGU (255), Journal article, 1968)Following brief notes on the low-grade metasediments occuring in the area near Hegra, 50 km east of Trondheim, the types of structures associated with three episodes of deformation of main Caledonian (Silurian) age are ... -
Tectonic setting of the Tronfjell Massif ; further evidence for pre-Scandian orogenesis in the Trondheim Nappe Complex, Central Norway.
(NGU Bulletin (434), Journal article, 1998)The Tronfjell Massif consists of layered mafic intrusion, containing dunites and olivine-bearing to noritic gabbros, lying within metasedimentary rocks of the Hummelfjell Group. The initially more or less flat form of the ... -
Tectonic succession of the Caledonian nappe front in the Haukelisæter- Røldal area, Southwest Norway.
(NGU (292), Journal article, 1973)It is concluded from reconnaissance studies on Hardangervidda that a succession of 5 allochthonous units occurs above the Precambrian basement and its autochthonous\/parautochthonous cover. The units are named from bottom ... -
Tectonostratigraphic succession and development of the Finnmarkian nappe sequence, North Norway.
(NGU (343), Journal article, 1978)Detailed investigations of the Finnmarkian nappe sequence within the 1:250 000 map-sheets \"Hammerfest\", \"Nordreisa\" and \"Honningsvåg\" have revealed a complex construction of discrete nappes, sub-nappes and minor ... -
Tectonostratigraphy in the Velfjord-Tosen region, southwestern part of the Helgeland Nappe Complex, Central Norwegian Caledonides.
(NGU Bulletin (421), Journal article, 1991)In the southwestern parts of the Helgeland Nappe Complex, dismembered ophiolites and their cover sequences are imbricated together with nappes consisting dominantly of continentally derived rock units. A local nappe sequence ... -
Tekst til geologisk kart over fjeldstrøkene mellem Jostedalsbræen og Ringerike
(NGU (47), Journal article, 1908)Forkortet: In the map a distinction has been made between the old Archaean which consists chiefly of granite and gneiss and the Telemark formation (Algonkian) which is colored yellow with red lines. White quartzite and ... -
Tekst til geologisk oversigtskart over det sydlige Norge
(NGU (70), Journal article, 1914)