Browsing Artikler by Title
Now showing items 972-991 of 1064
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The surface of the inland ice in the Atndalen valley, South-central Norway.
(NGU Bulletin (438), Journal article, 2001)On the basis of different field observations, several authors have discussed the form of the inland ice in southern Norway. In this work, lateral features indicating the upper limit of zones of meltwater drainage marked ... -
The Surna, Rinna and Orkla Nappes of the Surnadal-Orkdal district, southwestern Trondheim
(NGU Bulletin (418), Journal article, 1990)In the district between Surnadal and Orkdal within the 'Gula', the rock sequence between the Late Precambrian metasandstones of the Tingvoll Nappe and assumed Lower Ordovician metavolcanites of the Støren Nappe, three major ... -
The Sveconorwegian magmatic and tectonometamorphic evolution of the high-grade Proterozoic Flekkefjord complex, South Norway.
(NGU Bulletin (434), Journal article, 1998)The Precambrian Flekkefjord complex is situated in the core zone of the Sveconorwegian orogenic belt in south-western Norway, covering the transitional zone between the south Rogaland anorthosite province to the west and ... -
The tectonostratigraphic setting of stratabound sulphide deposits in the southern Trondheim region, Central Norwegian Caledonides.
(NGU Bulletin (412), Journal article, 1988)The large number of mainly massive, polymetallic, stratabound sulphide depositswithin the southern Trondheim region are spatially confined to the differentnappe units of the central Scandinavian Caledonides. The rocks of ... -
The Tectonostratigraphy and structural evolution of the Sitas Area, North Norway and Sweden (68°N).
(NGU Bulletin (416), Journal article, 1989)The Sitas area contains rock derived from the pre-Caledonian Scandinavian craton and from an accreted Caledonian fore-arc complex. These rocks form the par-authocthonous (?) Rombak Complex which can be tied stratigraphically ... -
The terrane concept and the Scandinavian Caledonides
(NGU Bulletin (413), Journal article, 1988)A revised terrane map is presented for the Scandinavian Caledonides, and an outline is given of the principal suspect and exotic terrane-complexes identified outboard from the Baltoscandian miogeocline. The outermost part ... -
The Tromsø-Lyngen glacier readvance (early Younger Dryas) at Hinnøya-Ofotfjorden, northern Norway: a reassessment
(NGU Bulletin (445), Journal article, 2005)Based on radiocarbon dates, marine seismic data, mapping of surficial deposits, observations of marine limits and shoreline correlations, we have documented a considerable glacier readvance during the Tromsø-Lyngen event ... -
The Ulriken Gneiss Complex and the Rundemanen Formation: a basement - cover relationship in the Bergen Arcs, West Norway.
(NGU Bulletin (412), Journal article, 1988)The Ulriken Gneiss Complex (UGC) and its sedimentary cover, the RundemanenFormation, have been investigated. The UGC is a Precambrian migmatite complexwhich suffered strong but heterogeneous reworking during the ... -
Thermal conductivities of some ores and rocks in Norway.
(NGU (300), Journal article, 1973)Thermal conductivities of 61 diamond core smples are given. Most of the samples are from the Joma pyrite deposit and its neighbouring rocks. The measurements from Joma show that there is a very high conductivity in compact ... -
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 ... -
Thickness, distribution and depositional environment of Holocene sediments in the Norwegian part of the Skagerrak
(NGU Bulletin (430), Journal article, 1996)A regional seismic reflector separating an uppermost low-reflectivity Holocene unit from an acoustically layered, Lake Weichselian, glaciomarine unit below has been mapped in the Norwegian Skagerrak between Langesund and ... -
Tidligere undersøkelser over opløseligheten av feltspatens kaliindhold og undersøkelser over kalifeltspat som kalikilde for planterne.
(NGU (108), Journal article, 1922) -
Timing and tectonic significance of Sveconorwegian A-type granitic magmatism in Telemark, southern Norway: New results from laser-ablation ICPMS U-Pb dating of zircon
(NGU Bulletin (447), Journal article, 2007)The ages of six Sveconorwegian A-type granites without penetrative deformational fabric and an intrusive rhyolite porphyry from Telemark, southern Norway, have been determined by laser ablation inductively coupled plasmasource ... -
Timing of late- to post-tectonic Sveconorwegian granitic magmatism in South Norway.
(NGU Bulletin (440), Journal article, 2002)Dating of late- to post-tectonic Sveconorwegian granitic intrusions from South Norway by the SIMS U-Pb method on zircons and by internal Pb-Pb isochrons on rock-forming minerals indicates a major event of granitic magmatism ... -
To leirfall frembragt ved bombeangrep.
(NGU (167), Journal article, 1946)The clay-slides by Brøther near Lillestrøm and by Fjellvik near Sandefjord are interesting by the circumstance that they are due to bomb explosions. By Brøther near the aerodrome of Kjeller a heavy allied bomb raid took ... -
Torv
(NGU (105), Journal article, 1922)Die grossen Schwierigkeiten in der Versorgung mit Brennmaterialen, unter denen unser Land w\u00CChrend des Weltkrieges zu leiden hatte, brachte auch die Torffrage wieder stark in den Vorgrund. Die Verwendung von Stichtorf ... -
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 ... -
Torvmyrernes lagdeling i det sydlige Norges lavland
(NGU (90), Journal article, 1922)Das Pflanzenleben der Moore, das seine Zusammensetzung in erster Reihe der Fuchtigkeit des Bodens verdankt, tr\u00CCgt in Norwegen doch auch stark das Gepr\u00CCge klimatischer Faktoren. Dies tritt deutlich hervor in dem ... -
Trace fossils in the Halkkavarre section of the Dividal Group (?late Precambrian - Lower Cambrian), Finnmark.
(NGU (288), Journal article, 1973)The increasing abundance of trace fossils in the ?late Precambrian to Lower Cambrian sediments of the Dividal Group is comparable with that found in the laterally equivalent but much thicker succession to the east and ... -
Trekk av isbevegelsen og isavsmeltningen i Nordre Gudbrandsdalens fjelltrakter.
(NGU (223), Journal article, 1963)Glacial striae and ice-moulded forms indicate that the earliest direction of glacial flow was towards E, and that the flow at the maximum was towards N or NW. The late-glacial movement, however, seems to have been towards ...