Browsing Artikler by Subject "MALMGEOLOGI"
Now showing items 21-40 of 44
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I. Fra indre Helgeland. Fjeldbygningen og bergartene samt bemerkninger om bergverksdriften
(NGU (59), Journal article, 1911)Forkortet: Helgeland, the southern part of the district of Nordland, it situated between about 65\u00B0 and 66 1\/2\u00B0 N. Some of the inner parts of this great district were the object of the author's investigations ... -
II. Geologiske iagttagelser fra nordvestsiden av Hardangerfjord
(NGU (59), Journal article, 1911)Forkortet:The region described is situated in Western Norway on the NW-side of theHardangerfjord between 60\u00B0 6' and 60\u00B0 40' N. At the close of the Ice Age theland lay lower than at present. Raised beaches and ... -
III. Kvartsstrøket mellem Bodø og Folden
(NGU (79), Journal article, 1917)It is a part of the coast-region in Northern Norway which is here described. It lies to the east of the Vestfjord between 67 degrees 20' and 67 degrees 40' N. The mountainous island of Landegode consists of granite. This ... -
IV. Nogen bidrag til Hitterens og Smølens geologi
(NGU (69), Journal article, 1914)Forkortet: Hitra and Smøla (Map on p.6) are two rather large islands on the West coast of Norway at 63 1\/2\u00B0N. Smøla belongs entirely to the coast plain of Norway and is remarkably low and flat. A great part of Hitra ... -
Jordbunden i Romsdals amt. Del 1. Den almindelige del og herrederne i søndmør
(NGU (18), Journal article, 1895) -
Kart-katalog over Norges berggrunn. Catalogue of maps, bed-rock geology of Norway.
(NGU (193), Journal article, 1956) -
Kongsberg-Bamble formasjonen
(NGU (146), Journal article, 1936)A prominent friction breccia running from Modum in north to Kristiansund in south divides the pre-Cambrian of Southern Norway into two parts that differ markedly in their geology, petrography, metamorphism and ore deposits. ... -
Kongsbergfeltets geologi.
(NGU (82), Journal article, 1917)Kongsberg is situated about 80 km west of Oslo at the river Numedalslågen. On p. 8 may be seen a list of the rocks, which occur in the region. All these rocks are of Precambrian age. Besides, there occur dykes of diabase, ... -
Lofoten og Vesteraalen
(NGU (23), Journal article, 1897) -
Narvik. Beskrivelse til det berggrunnsgeologiske gradteigskart N9 - 1:100 000 (med fargetrykt kart).
(NGU; Skrifter (308; 13), Journal article, 1974)The geological map Narvik, published in 1950, is briefly described. The bedrock of this map area can be subdivided into autochthonous and allochthonous rocks. The autochthonous rocks comprise the Precambrian (mainly the ... -
Nogle bemerkninger om Nordlands amts geologi
(NGU (4), Journal article, 1891)Forkortet: The two first landscapes are from the granite mountains of Lofoten. The illu- stration p.141 shows the gabbro mountain Sulitjelma. The illustrations p.142, 145 are from the region of the Cambrian-Silurian schists. ... -
Nogle bemerkninger om Tromsø amts geologi. (Efter Karl Pettersens arbeider)
(NGU (4), Journal article, 1891)Forkortet: This paper contains an explanation of the points where Pettersen differs from Dahll regarding the supposed Cambrian-Silurian schists. The illustrations p. 114, 115 are from the great mountain chain of gabbro to ... -
Nogle notiser fra Sigdal og Eggedal
(NGU (37), Journal article, 1904)Forkortet: The valley of Sigdal (dal means valley) with its continuation in Eggedal are situated to the West of Christiania in Southern Norway. The rocks are Archaean gneiss and granite with some gabbro. At the northwestern ... -
Norges geologiske undersøgelses udstilling i Bergen 1898
(NGU (26), Journal article, 1898)\"Kart over Norges malmforekomster\" med grafisk fremstilling af \"Norges bergverksdrift 1850-97\" av Johan H.L.Vogt. Kart over Norges sten- og mineralindustri av Carl F.Kolderup. -
Norsk marmor
(NGU (22), Journal article, 1897)Forkortet: Diese Arbeit zerf\u00E4llt in vier Hauptabschnitte. 1. \u00DCber die Geologie des Marmors (S.4-18). 2. \u00DCber die wichtigsten Eigenschaften des Marmors, mit besonderer R\u00FCcksicht auf die norwegischen ... -
Radioaktivitetsundersøkelse av bergartsprøver i magasinene på Mineralogisk geologisk museum, Universitetet i Oslo.
(NGU (213), Journal article, 1961)The radioactivity of 5813 specimens from about 25% of the ore deposits registered by Foslie in NGU nr. 126, 1925, have been measured by gamma-scintillation-counter. Anomalies have been found in specimens from about 40 ... -
Rennebu. Fjeldbygningen inden rektangelkartet Rennebus omraade
(NGU (56), Journal article, 1910)Forkortet: The Rennebu sheet embraces an area of about 590 square miles, situated about 28 miles south of Trondheim. Professor Tørnebohm (p.6) and Professor Kjerulf (p.6) have each given their view of the geological ... -
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 Søndhordland og Ryfylke
(NGU (64), Journal article, 1913)Forkortet: The first section deals with the previous literature on the subject. The geology of the region of the high mountains and the fjords. This region comprises the whole area represented on our map with exception of ... -
The Early Proterozoic Karasjok Greenstone Belt, Norway. A preliminary description of lithology, stratigraphy and mineralization.
(NGU Bulletin (403), Journal article, 1985)The Karasjok Greenstone Belt of Finnmark, Norway, is a sequence of medium-grademetmorphic supracrustal rocks in the northernmost part of the Baltic Shield.Regional mapping has revealed a tectonostratigraphy with the ...