Browsing Artikler by Title
Now showing items 321-340 of 1064
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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 ... -
Geothermal aspects of hydrocarbon exploration in the North Sea area.
(NGU (316), Journal article, 1975) -
Glacial geology of the area between Jostedalsbreen and Jotunheimen, South Norway.
(NGU (291), Journal article, 1973)Ice movement and the course of deglaciation are reconstructed. The age of and the climate during the deglaciation are discussed in the light of equilibrium line displacement, shoreline positions, pollen analysis and ... -
Glacial geology of Western Troms, North Norway.
(NGU (256), Journal article, 1968)A moraine chronology was established for western Troms. Altogether six main glacial phases were recognised. Several of the phases were radiocarbon dated. Observations were made of the corresponding shore lines, the marine ... -
Glacial geology,deglacition chronology and sea-level changes in the southern Telemark and Vestfold counties, Southeastern Norway
(NGU Bulletin (435), Journal article, 1999)A revised and more detailed deglaciation chronology is presented in the soputhern Telemark and Vestfold, southeastern Norway, based mainly on information and results from mapping projects on the superficial deposits carried ... -
Glacial stadials and interstadials of the Late Precambrian Smalfjord Tillite on Laksefjordvidda, Finnmark, North Norway.
(NGU (358), Journal article, 1980)Three glacial conglomerates and two intervening sandstones in the Smalfjord Formation on Laksefjordvidda were deposited during three glacial episodes and two interstadials, respectively. MOst of the sequence is preserved ... -
Glasialgeologi og vegetasjonsinnvandring i Indre Nordhordland, Vest-Norge.
(NGU (369), Journal article, 1981)In the area between Hardangerfjorden and Sognefjorden an oldest regional ice movement towards the west has been reconstructed. Younger regional ice movements were towards south-west in the southern parts. Therefore, an ... -
Glidning av Arnebråtveien nr. 30.
(NGU (166), Journal article, 1946)At Arnebråtveien 30 in Aker a sliding of the clayey ground occurred in the evening of May 29th 1936. A road had been built on a foundation of stone. The ground was too weak to stand the weight of the ballast. By a sliding ... -
Glidning og ras av jernbanefyllinger 16-19 april 1937.
(NGU (166), Journal article, 1946)During these days a remarkable number of slides damaged Norwegian railways. April 16th a sandy railway ballast slid out near Skotselv station between Hokksund and Hønefoss. 5000 m3 of ballast slid into the Drammen river, ... -
Glimmermineralernes betydning som kalikilde for plantevern
(NGU (108), Journal article, 1922)Denne avhandling inneholder en undersøkelse over oppindelsen av jordbundens kaliindhold, eller nærmere præcisert den del av jordbundens kaliindhold som kan tilgodegjøres av planterne.Hittil har man som regel gaat ut fra, ... -
Globulith, a new type of intrusive structure, exemplified by metabasic bodies in the Moss area, S.E. Norway.
(NGU (266), Journal article, 1970)Intrusion of basic magma into a regionally preheated gneiss complex has given rise to oddly shaped, globular to botryoidal, intrusions with associated contact anatexis and contact deformation whereby pseudoconcordant ... -
Granåsen, a dolomite-brucite deposit with potential for industrial development.
(NGU Bulletin (436), Journal article, 2000)Granåsen, situated close to Mosjøen in northern Norway, is a deposit containing several million tonnes of dolomite and brucite. The deposit has been investigated and characterised in preparation for future development and ... -
Granite pegmatite quartz from Evje-Iveland: trace element chemistry and implications for the formation of high-purity quartz
(NGU Bulletin (436), Journal article, 2000)Previous studies imply that granite pegmatites and hydrothermal quartz veins are the most promising igneous repositories of high-purity quartz. This is because quartz from higher temperature geological settings (granites, ... -
Granite studies I. A gravity investigation of two Precambrian granites in South Norway.
(NGU (214B), Journal article, 1963)The Bouguer gravity anomaly map, based on 778 stations, covers the Precambrian rocks along the southeast coast of Norway from the Oslo region to Kristiansand. The principal features of the map are the low gravity gradient ... -
Granite studies II. The Precambrian Flå granite, a geological and geophysical investigation.
(NGU (219), Journal article, 1963)The Flå granite is composed of two adjacent elliptical granite bodies, the larger northern Hedal granite and the Ådal granite. The granites are surrounded by banded granodioritic gneisses. Migmatites and augen gneisses are ... -
Granitindustrien ved Idefjorden
(NGU (1), Journal article, 1891)Forkortet: The Iddefjord is the south-eastern part of Norway at the Swedish border. The granite there is of middle grain and gray (sometimes a little reddish). The rock is to a certain degree cleavable in two directions, ... -
Graptolitførende skifere i vestre Gausdal.
(NGU (1), Journal article, 1891)Forkortet:The Vestre Gausdal is situated in the central part of Southern Norway, 145 kmnorth of Oslo. It lies on the border-zone between the sparagmite-formation,which is Cambrian, and the overlying Silurian schists, which ... -
Gravel fraction on the Spitsbergen Bank, NW Barents Shelf.
(NGU (316), Journal article, 1975)The gravel fraction of the bottom sediment on the Spitsbergen Bank, located south of Svalbard in the NW Barents Sea, is composed predominantly of clastic sedimentary rocks, especially sandstone and shale. Betwwen sampling ...