NGU-publikasjoner: Nye registreringer
Viser treff 661-680 av 7138
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The geology between Salangsdalen and Gratangenfjord, Troms, Norway.
(NGU Bulletin (405), Journal article, 1986)Forkortet.The geology of an area in southernmost Troms, Norway is presented. SevenCaledonian nappe are recognised, and these rest with thrust contact abovePrecambrian crystalline basement. -
A Late Quaternary correlation chart for Norway.
(NGU (223), Journal article, 1963)A correlation chart is presented containing the stratigraphical results of some selected Norwegian studies in the wide field of Quaternary geology. Studies of plant remains in bogs, pollen investigations, evidence of ... -
Om glimmermineralernes deltagelse i jordbundens kalistofskifte og om disse mineralers betydning for landbruket.
(NGU (108), Journal article, 1922) -
Evaluation of sand and gravel in Finnmark as a guide to locating deposits suited to building purposes.
(NGU Bulletin (403), Journal article, 1985)Forkortet. Bedrock mapping and investigations of rock-types in Finnmark as well as else- where in Norway have made it possible to classify the components by their strength or mechanical properties. Three categories of ... -
Norges geologiske undersøkelse. Årsberetning for 1961.
(NGU (215), Journal article, 1962) -
A possible basement to the Mesoproterozoic quartzites on Hardangervidda, South-Central Norway: zircon U-Pb geochronology of a migmatitic gneiss
(NGU Bulletin (437), Journal article, 2000)On Hardangrvidda west of the Mandal-Ustaoset fault zone in South Norway, some 80-90% of the crust consists of orthogneisses and foliated and massive granites in this plutonic environment the Mesoproterozoic quartzites of ... -
Mineral characterisation of industrial mineral deposits at the Geological Survey of Norway: a short introduction
(NGU Bulletin (436), Journal article, 2000)Mineral characterisation involves the study of minerals in terms of their size, habit, chemical composition, morphology, textural position, association and other attributes. There is an established and increasingly important ... -
Depth of extensional faulting on the Mid-Norway Atlantic passive margin.
(NGU Bulletin (437), Journal article, 2000)Two crustal-scale cross-sections of the Mid-Norwegian Atlantic passive margin are discussed. Large W- and E-dipping normal faults relate to extension of the continental crust following the Caledonian orogeny and the ... -
C14-datings referring to shore lines, transgressions, and glacial substages in Northern Norway. (A supplement to papers of 1960 and 1961 by the author).
(NGU (215), Journal article, 1962)Denne publikasjonen er en foreløpig meddelelse som i det vesentlige dreier seg om en serie C14-dateringer utført av R. Nydal ved Laboratoriet for Radiologisk Datering i Trondheim. Dateringene synes å gi viktige opplysninger ... -
Stratigraphy and structure of the Ringebu - Vinstra district, Gudbrandsdalen; with a short analysis of the western part of the sparagmite region.
(NGU (293), Journal article, 1973)The Ringebu-Vinstra district, Gudbrandsdalen, is one in which several of the main structural units in Southern Norway come together. Essentially, the rocks belong to three main tectonic units: 1. Parautochthonous rocks of ... -
Basement-cover relations and Caledonian tectonostratigraphy of Sandsøya, Grytøya, Åkerøya and Kjøtta, Western Gneiss Region, North Norway.
(NGU Bulletin (431), Journal article, 1996)Rocks of Sandsøya, Grytøya, Åkerøya, and Kjøtta, represent four Caledonian Tectonic settings: (1) pre-Caledonian Baltic crystalline basement of the Western Gneiss Region, including intrusively enclosed supracrustal rocks; ... -
The Nickeliferous Iveland-Evje amphibolite and its relation.
(NGU (168a), Journal article, 1947)The pre-Cambrian nickelferous meta-norite at Iveland-Evje represents an amphibolite body entirely surrounded by gneissous granite and augen genisses. More than 90% of the amphibolite body is made up with schistose or ... -
Torvmyrer inden kartbladet "Sarpsborgs" omraade
(NGU (5), Journal article, 1891)The peatmosses studied occur on the eastern side of the Oslofiord in the environs of the small town of Sarpsborg. The first part of the paper contains the description of the individual mosses. The numbers upon the table ... -
Composition of metamorphic rocks and some aspects of evolution of the Lapland Granulite Belt on the Kola Peninsula, USSR
(NGU Bulletin (421), Journal article, 1991)Combined geological and petrochemical data suggest that the Lapland Granulite Belt can be divided into a lower sedimentary-volcanic unit and an upper, predominantly sedimentary sequence. Metamorphic rocks from the lower ... -
Leirfallet ved Lade, Trondheim 1944. Foredrag holdt i Norsk Geologisk Forening 11.4.1945
(NGU (167), Journal article, 1946)On April 11. 1944 a clay-slide took place near Ladehammeren N of Trondheim. About 5 acres of the field between Lade Alle and the Ladebekken streamlet slid down. Liquid clay was not visible. There was great uncertainty about ... -
Results of recent geological and geophysical investigations in Moray Firth, Scotland.
(NGU (316), Journal article, 1975)Geophysical, shallow drilling and sea-bed sampling investigations have shown that the main sedimentary basin of the Moray Firth is separated by an ENE-trending, horst-like uplift zone from a secondary basin to the south. ... -
Norges hevning etter istiden
(NGU (96), Journal article, 1922)The present paper is in substance an explanatory text accompanying a map of the post-glacial changes of level in the Scandinavian peninsula. At the end of the Glacial Period the Scandinavian peninsula was more deeply ... -
V. Om Andøens jurafelt, navnlig om landets langsomme nedsynken under juratiden og den senere hævning samt gravforkastning
(NGU (43), Journal article, 1905)Forkortet:Das Andøya Jurafeld, das auf der Strandebene (s. Fig.1,4 und Tafel I.Profil Fig.1 und 2) liegt, hat eine L\u00E4nge von ca. 8.4 Km und ein Areal auf festem Lande von etwa 10 km\u00B2; das Areal muss aber noch ... -
A preliminary account of the geology of the Signaldalen-Upper Skibotndalen area, Inner Troms, N. Norway.
(NGU (247), Journal article, 1967)A preliminary account of the petrography, stratigraphy and structure of an area at the Caledonian front in inner Troms, N. Norway, is given. Precambrian autochthonous gneisses are overlain by autochthonous and par-autochthonous ... -
Disparate geochemical patterns from Snåsavatn greenstone, Nord-Trøndelag, Central Norway.
(NGU (373), Journal article, 1982)Greenstone volcanites of Middle Ordovician age from the Snåsavatn area of the Central Norwegian Caledonides can be divided into two distinctive groups on the basis of their geochemical patterns. The bulk of the lavas sampled ...