Blar i NGU-publikasjoner på emneord "BERGGRUNNSGEOLOGI"
Viser treff 621-640 av 698
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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 ... -
Terminal Proterozoic System. Fieldguide to the workshop in Eastern Finnmark, North Norway, 1-8 August 1994
(NGU-Rapport (94.065), Report, 1994)Ekskursjonsfører med beskrivelse av utvalgte lokaliteter og snitt i Varangerfjorden og Tanafjorden områdene -
Terrænundersøgelser og jordboringer i Stjørdalen, Værdalen og Guldalen samt i Trondhjem i 1894, 95 og 96
(NGU (27), Journal article, 1898)Forkortet: The Norwegian valleys filled up at a large extent by gravel, sand and clay in the course of time been submitted to earthslips and sinking of the grounds, however more especially those of Gauldalen, Stjørdalen ... -
The copper deposits of the Birtavarre district, Troms, Northern Norway. Kopperforekomster i Birtavarre-området Troms.
(NGU (199), Journal article, 1957)The report gives the results of a 4-year (1952-55) programme for the investigation of a former copper-mining area in the north of Norway, carried out by the Geological Survey of Norway (NGU). The stratigraphy and structure ... -
The Fongen - Hyllingen layered intrusion, Trondheim region, Norway: an excursion guide
(NGU-Rapport (2010.015), Others, 2010)The Fongen-Hyllingen complex, situated 60 km southeast of Trondheim, Norway, comprises the 160 km2 Fongen-Hyllingen layered mafic intrusion (FH1) and the slightly younger, minor (3 km2) mafic to ultramafic Treknattan ... -
The Fongen-Hyllingen Complex. Berggrunnskart 1:30 000
(Map, 2008) -
The geological evolution of the North Sea area in the tectonic framework of North Western Europe.
(NGU (316), Journal article, 1975)The development history of the North Sea area can be subdivided into five stages: 1) Caledonian geosynclinal stage (Cambrian-Silurian), 2) Variscan geosynclinal stage (Devoanin-Carboniferous), 3) Permo-Triassic intracratonic ... -
The geological interpretation of the Slidre positive gravity anomaly.
(NGU (228), Journal article, 1964)A positive gravity anomaly that occurs in Slidre has an amplitude of 53 mgal and can be separated into two parts. The top of the disturbing body causing the anomaly cannot be deeper than 4 km. Gabbros and mafic gneisses ... -
The geology of the Vaddas area, Troms: a key to our understanding of the Upper Allochthon in the Caldonides of northern Norway
(NGU Bulletin (445), Journal article, 2005)The Vaddas area in the North Norwegian Caledonides is underlain by the Corrovarri Nappe, the uppermost unit of the Kalak Nappe Complex, and the overlying Vaddas Nappe representing the lowermost unit of the Reisa Nappe ... -
The lead and zinc bearing veins at Tråk in Southern Norway.
(NGU (250 B), Journal article, 1967)The nearly vertical zinc and lead bearing veins that cut through Precambrian rocks near the Oslo region at Tråk in Bamle Southern Norway, are described. They can be followed for nearly 2.5 km. A younger introuded diabase ... -
The Lofoten-Lopphavet Project - an integrated approach to the study of a passive continental margin, Summary report
(NGU-Rapport (93.129), Report, 1993)An integrated study of geophysical data from the offshore and onshore areas of northern Norway between 67\u00B0 and 71\u00B0N was carried out as a collaboration project between Elf Petroleum, Norsk Hydro, The Norwegian ...