Browsing Artikler by Title
Now showing items 828-847 of 1064
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Structure and evolution of the Atlantic floor between Northern Scotland and Iceland.
(NGU (316), Journal article, 1975)The continental shelf west of the Shetland and Orkney islands is a region of varied geology traversed by the Caledonian front, including some areas of shallow basement and some partially fault-bounded Mesozoic basins such ... -
Structure and petrology of the Bergen-Jotun kindred rocks from the Gjendebu region, Jotunheimen, Central Southern Norway.
(NGU (373), Journal article, 1982)The Gjendebu region is located within the Jotun Nappe, highest tectonic unit of the southern Norwegian Caledonides. The structure of the area is dominated by the NE-rending Tyin-Gjende Fault, a major zone of repeated ... -
Structures and metamorphism at Brygfjell-Simafjell within the Rødingsfjellet Nappe Complex, Nordland, Norway
(NGU Bulletin (431), Journal article, 1996)Structures and metamorphic featues are described from parts of the area of 1:50 000 map-sheet Korgen. The area investigated is situated within the Rødings- fjellet Nappe Complex in the Caledonides of Nordland. The rocks ... -
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 ... -
Studies in the Trondheim region, Central Norwegian Caledonides
(NGU (227), Journal article, 1964) -
Studies in the Trondheim Region, Central Norwegian Caledonides II
(NGU (245), Journal article, 1967) -
Studies on the Latest Precambrian and Eocambrian Rocks in Norway
(NGU (238), Journal article, 1966) -
Studies on the latest precambrian and Eocambrian rocks in Norway
(NGU (251), Journal article, 1967) -
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 ...