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Geology of the Båtsfjordfjellet drillcore, Varanger Peninsula, Finnmark, northern Norway
(NGU Bulletin (452), Journal article, 2012)Logging of >800 metres of drillcore from a borehole on Båtsfjordfjellet, Varanger Peninsula, revealed a succession of very low-grade, metasedimentary rocks which are assigned to specific Neoproterozoic formations recognisable ... -
Geology of the eastern part of the Meråker area.
(NGU (245), Journal article, 1967)Within the mapped area slightly metamorphosed clastic sediments occur, probably of Upper Ordovician and Silurian age. The author describes a metagreywacke-slate association with metaconglomerates and gabbrodiorite sills, ... -
Geology of the Folldal area, southern Trondheim Region Caledonides, Norway.
(NGU Bulletin (426), Journal article, 1994)The lowest stratigraphic unit in the Folldal area is the Gula Group, comprising turbidites and minor greenstones in the lower part (the Singsås Formation) and graphitic pelites with subordinate marble and conglomerate in ... -
Geology of the Hølonda-Hulsjøen area, Trondheim region.
(NGU (266), Journal article, 1970)The geology of the area south of Trondheim is described. A new stratigraphical division of the Early Palaeozoic is proposed and its structure outlined. The entire Early Palaeozoic sedimentary and volcanic complex has been ... -
Geology of the Iesjav'ri-Skoganvarre area, Northern Finnmarksvidda, North Norway.
(NGU Bulletin (403), Journal article, 1985)The Iesjav'ri-Skoganvarre areas is located in the northern part ofFinnmarksvidda and its underlain by Archaean-Early Proterozoic rocks. Theoldest unit, the Jer'gul Gneiss Complex, is unconformably overlain bymetasediments ... -
Geology of the Meråker area as a key to the eastern part of the Trondheim region.
(NGU (245), Journal article, 1967)The present paper deals with a discussion of the main tectono-stratigraphical problems of the eastern Trondheim region. Based on detailed studies made in the Meråker area in the last three summers and available manuscript ... -
Geology of the Meråker area. Introduction.
(NGU (245), Journal article, 1967) -
Geology of the Minor Bergen Arc, West Norway.
(NGU Bulletin (416), Journal article, 1989)Detailed mapping of the Minor Bergen Arc has revealed the presence of a variety of highly deformed rocks of different origin and age. Three rock units have been separated and named. The Nordåsvatn Complex comprises deformed ... -
Geology of the Mostadmarka and Selbustrand area, Trøndelag.
(NGU (232), Journal article, 1965)The bedrock of the area consists of metamorphic epiclastic, volcanic, and intrusive rocks of assumed Lower Ordovician age, assigned to, and lithologically matching the rocks of, the Røros, Støren and Lower Hovin Groups of ... -
Geology of the northernmost part of the Meråker area.
(NGU (245), Journal article, 1967)Four lithostratigraphical groups comprising sedimentary and igneous rocks have been distinguished in the mapped area. There are conformities and gradual transition between all these groups. The rocks have been subjected ... -
Geology of the Røssjøkollan-Dokkvatn area, Oppland.
(NGU (314), Journal article, 1974)The Røssjøkollan-Dokkvatn area at the eastern edge of Valdres Sparagmite exposures is comprised of a number of allochthonous litho-tectonic units in which Precambrian Jotun basement, and Late Precambrian or Eocambrian ... -
Geology of the Skrukkelia molybdenite deposit, northwest margin of the Oslo Graben, Norway.
(NGU (387), Journal article, 1983)The Skrukklia Mo-occurence is situated in Precambrian gneisses along the northwest margin of the igneous complex of the Oslo Region. Within the mineralized area a Permian granite suite (the Aurtjern granite) intrudes the ... -
Geology of the southern part of the Kautokeino Greenstone Belt: Rb-Sr geochronology and geochemistry of associated gneisses and late intrusions.
(NGU Bulletin (403), Journal article, 1985)The southern part of the Kautokeino Greenstone Belt is divided into four volcanic formations separated by sedimentary units. The formation represent a development from Archaean komatiitic sequences to Middle Proterozoic ... -
Geology of the West Troms Basement Complex, northern Norway, with emphasis on the Senja Shear Belt: a preliminary account.
(NGU Bulletin (427), Journal article, 1995)Frie emneord: Diabasganger -
Geology of the western and north-eastern part of the Meråker area.
(NGU (245), Journal article, 1967)A thick metasedimentary sequence together with a volcanic and hypabyssal intrusive complex is described. While strata dip generally westwards it can be shown that the succession is, for the most part, inverted; the discovery ... -
Geology of three dioritic plutons in Velfjord, Nordland.
(NGU Bulletin (423), Journal article, 1992)Dioritic plutons in the Velfjord area of Nordland intrude calc-silicates and migmatitic pelites of the Helgeland Nappe Complex (HNC). The three largest plutons were emplaced in a zone of NNW-SSE regional strike rather than ... -
Geometry and kinematics of extensional deformation along the northern edge of the Rombak Window, Nordland, North Norway.
(NGU Bulletin (415), Journal article, 1989)Deformation along the northern edge of the Rombak Window documents an unusual extensional event during the evolution of a colliosional orogen. The extension occurred along a series of ductile deformation zones that strike ... -
Geometry and vertical extent of the late Weichselian ice sheet in northwestern Oppland County, Norway
(NGU Bulletin (451), Journal article, 2011)The position of the ice margin during the last deglaciation is well known in Scandinavia, in particular during the Younger Dryas (YD) chronozone from when large ice marginal deposits easily can be traced at or close to the ... -
Geophysical and geological interpretation of regional structures within the Precambrian Kautokeino Greenstone Belt, Finnmark, North Norway.
(NGU Bulletin (403), Journal article, 1985)The Kautokeino Greenstone Belt comprises a synclinorium of volcano-sedimentary rocks. This sequence of Early Proterozoic age is situated between two culminations of gneisses. Large areas of the belt have been mapped in ... -
Geophysical measurements in Jeløya.
(NGU (247), Journal article, 1967)As a part of geological\/geophysical student field courses a series of magnetic and gravimetric observations has been carried out at Jeløya. Geological samples have been collected and the physical properties of the samples ...