NGU-publikasjoner: Nye registreringer
Viser treff 241-260 av 7138
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Kart-katalog over Norges berggrunn. Catalogue of maps, bed-rock geology of Norway.
(NGU (193), Journal article, 1956) -
Årsberetning for 1969
(NGU (266), Journal article, 1970) -
Kisdistriktet Varaldsøy-Ølve i Hardanger og bergverksdriftens historie.
(NGU (147), Journal article, 1955)When Steinar Foslie suddenly passed away in november 1951, he had finished the geological map here presented: \"Kisdistriktet Varaldsøy-Ølve i Hardanger\", based on field-work during 1942-49. Furthermore his M.S. contained ... -
Development of minor late-glacial ice domes east of Oppdal, Central Norway
(NGU Bulletin (441), Journal article, 2003)Glacial striations and ice-marginal forms such as lateral moraines and meltwater channels show that a major north-westerly-directed ice flow invaded the Oppdal area prior to the Younger Dryas (YD) Chronozone. Through the ... -
Meta-andesites in the Caledonides in the Suldal area, Ryfylke.
(NGU (288), Journal article, 1973)Meta-andesites interlayered with quartz-mica schists, phyllites and tuffites of supposed Cambro-Silurain age cover an area of about 120 km2 in the Suldal area, Ryfylke. Recrystallized meta-andesites are also found in the ... -
The geology and petrology of the Rognsund intrusion, West Finnmark, Northern Norway.
(NGU (371), Journal article, 1982)The Rognsund intrusion is an early-Caledonian gabbroic body containing an 800 m thick sequence of metamorphosed cumulates. Well-developed rythmic layering is interpreted in terms of both in situ crystallization and deposition ... -
Beskrivelse til berggrunnsgeologisk kart over strøket Agdenes- Hemnefjord, Sør-Trøndelag.
(NGU; Skrifter (299; 9), Journal article, 1974)The area consists of regional metamorphic gneisses and crystalline schists. Some of the rocks are of Cambrian-Ordovician age, others of Precambrian age. Examples on the former are flagstones (metamorphosed \"sparagmite\") ... -
Geologisk beskrivelse til Nordlandskartet
(NGU (70), Journal article, 1914) -
Leirfall ved Holund i Grong 1942.
(NGU (167), Journal article, 1946)On january 19th, 1942 a violent clay-slide took place near the farm Holund in Grong district, east of Namsos. The size of the displaced area was about 1 acre. A heavy wave of liquid clay rushed down into a small valley. ... -
The relation between the basal gneiss and the overlying meta-sediments in the Surnadal district, (Caledonides of Southern Norway).
(NGU (184), Journal article, 1953)The boundary between the basal gneiss and the overlying micaschists and micaceous gneisses is marked by a thin zone of \"basal quartzite\", but the quartzite is generally not at the exact boundary between the two divisions. ... -
Isbevegelse i Lillehammer-området, Sør-Norge, under siste nedising.
(NGU (378), Journal article, 1983)The ice movement from the last glaciation in the northern part of the lake Mjøsa district are presented in an ice phase model. Four main ice phases are reconstructed mainly based on striation, but fluted surfaces, poorly ... -
Recent observations on the southern shore of Skjervøy and the opposite coast of Kågen.
(NGU (255), Journal article, 1968) -
Norsk arsenmalm og arsenikfremstilling
(NGU (106), Journal article, 1922)The present paper is published by NGU as a report from \"Statens Raastofkomite\" on the emergency production of arsenic during the war when the supplies, ordinarily imported, were cut off. The paper also contains a synopsis ... -
The Caledonian mountain chain of the Southern Troms and Ofoten areas. Part I. Basement rocks and Caledonain meta-sediments.
(NGU (239), Journal article, 1966)The geology of the present area will be treated in a series ofthree publications. In the first paper the petrography and generalfeatures of the Precambrian rocks and the so-called \"basal gneisses\"are described and the ... -
Rb-Sr age of the Blåfjellhatten granite in the Olden Window, Central Norway.
(NGU Bulletin (420), Journal article, 1990)Rb-Sr isotope whole-rock dating of undeformed and unaltered parts of the Blåfjellhatten granite has yielded an isochron age of 1356 +- 29 Ma with I.R.=0.7254 +-0.0027, interpreted as the age of intrusion. This age contrasts ... -
Planktonic, acid-resistant microfossils from Upper Proterozoic strata of the Barents Sea Region of Varanger Peninsula, East Finnmark, Northern Norway.
(NGU (382), Journal article, 1983)Planktonic, acid-resistent microfossils (acritarchs) occur in the Kongsfjord, Båsnæring and Båtsfjord Formations of the Barents Sea Group and in the Styret Formation of the Løkvikfjell Group. Two new taxa are described and ... -
Benthic foraminiferal evidence of environmental change in the Skagerrak over the past six decades
(NGU Bulletin (430), Journal article, 1996)High resolution analyses of fossil benthic forminiferal assemblages have been performed on two short (<40cm) sediment cores from the deep Skagerrak Basin, NE North Sea. 210 Pb-datings of replicate cores from the same two ... -
Lead-zinc hydrothermal mineralization in the Pechenga Area, Kola Peninsula, Russia
(NGU Bulletin (423), Journal article, 1992)The Early Proterozoic Pechenga supracrustal belt in the western part of the Kola Peninsula, Russia contains hydrothermal Pb-Zn mineralizations, occurring as veins or sulphide disseminations along hydrothermally altered ... -
I. Den hvite granit i Sogn, geologisk optræden og tekniske egenskaper
(NGU (68), Journal article, 1913)Forkortet: The white granite of Sogn in Western Norway, although for many years known and repeately called attention to be geologists, has only recently come into use as a building material to any extent. In this paper is ... -
Thickness and distribution of sedimentary rocks in the southern Barents Sea.
(NGU (316), Journal article, 1975)The southern Barents Sea is underlain by sediments of varying thickness and physical properties. The thick sequence of Tertiary sedimentary rocks, which is representative of the southern provinces of the Norwegian continental ...