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Sub-till sediments at Rokoberget, Southeastern Norway
(NGU Bulletin (424), Journal article, 1993)A dark blue-grey, silty clay below till is described from a locality 230 m a.s.l. in the Rokosjøen depression east of Mjøsa. The sediment is glacially deformed but interpreted to represent a deposit from a period with local ... -
Subdivision of the Jotun Nappe Complex between Aurlandsfjorden and Nærøyfjorden, South Norway.
(NGU (380), Journal article, 1983)In the area between Aurlandsfjorden and Nærøyfjorden the Jotun Nappe Complex can be subdivided into a lower thrust unit of mainly gneisses with mangerites, jotunites and minor supracrustals (the Flåm unit), and an upper ... -
Subduction-related volcanism in the Gula Nappe, southeastern Trondheim Nappe Complex, Central Norway
(NGU Bulletin (428), Journal article, 1995)Field and geochemical evidence from two meta-igneous complexes that occur in the Einunnfjellet-Savalen area, southeastern Trondheim Nappe Complex, indicates that both complexes formes in an arc-related setting. Metabasalts ... -
Subsidence and tectonics in Late Precambrian and Palaeozoic sedimentary basins of southern Norway.
(NGU (380), Journal article, 1983)The assumption that sedimentary basins approach isotopic equilibrium provides a good foundation for modelling basin subsidence based on variables such as cooling rates (thermal contraction), crustal thinning, eustatic ... -
Suldalsfjeldene
(NGU (36), Journal article, 1903)Forkortet: The high mountain region round the Suldal lake to the NE of Stavanger in Southeastern Norway forms a continuation of the region described by Bjørlykke, Rekstad and Reusch in the \"Aarbog\" (Yearbook) of 1902. ... -
Sulitelmafeltets geologi og petrografi. Første del av et arbeide om Sulitelmafeltets fjellgrunn og malmforekomster.
(NGU (121), Journal article, 1927)The present publication is the first part of a monograph on the Sulitjelma district, containing the sections on physiography, general geology and petrology. In the second part the ore dposits will be described and their ... -
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 ... -
Sulphur isotope composition of the sandstone-lead deposits in southern Norway.
(NGU (380), Journal article, 1983)Samples of galena, pyrite and barite from the Norwegian sandstone-lead occurences in the Gjøvik area and at Osen and Galåa have been analyzed for their sulphur isotope composition. Samples from the Vassbo and Laisvall ... -
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 ...