Blar i NGU Open Archive på emneord "KARTLEGGING"
Viser treff 41-60 av 518
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Bidrag til Finmarkens geologi
(NGU (84), Journal article, 1918)The present paper is a result of investigations carried out in the most northern district of Norway, during the summers 1914-17, the total amount of time spent in Finnmark being 23 weeks. The studies have been confined to ... -
Big boulders of tillite rock in Porsanger, Northern Norway.
(NGU (247), Journal article, 1967)In 1959 numerous erratic boulders of tillite rock were discovered at the head of Austerbotn, the eastern arm of the Porsangerfjord. Some of the boulders are very big, having volumes of up to 20m3. In 1965 another two ... -
Biotitt-søvitt på Stjernøy, Vest-Finnmark.
(NGU (183), Journal article, 1952)The island of Stjernøy is built up of a complex of gabbroid rocks, which in the valley of Fjellfinndalen (fig. 1) surrounds a body of chiefly calcite-biotite rock more than commonly rich in apatite, clearly of non-sedimentary ... -
Brerandstadier og avsmeltingsforhold i Repparfjord-Stabbursdal- området, Vest-Finnmark. En deglaciasjonsprofil fra fjord til vidde.
(NGU (213), Journal article, 1961)The purpose of this article is given a description of two prominent active substages of the deglaciation period of the last ice-age in Finnmark, Northern Norway. The area concerned is situated on the peninsula between the ... -
Børgefjell. Beskrivelse til det berggrunnsgologiske gradteigskart J.19 - 1: 100 000
(NGU; Skrifter (298 ; 8), Journal article, 1973)Three main structural units are present: 1. The Precambrian (Svecofennokarelian) basement of the Børgefjell Window. \". Low grade (greenschist facies) Lower Paleozoic rocks belonging to the Seve-Køli Nappe Complex. 3. The ... -
Caledonian structural geology and tectonics of East Hinnøy, North Norway.
(NGU Bulletin (396), Journal article, 1984)Rocks of east Hinnøy comprise three Caledonian tectonic elements: (1) parautochthonous pre-Caledonian crystalline basement (Lofoten block); (2) allochtonous Precambrian gneisses, probably derived from the Lofoten block, ... -
Caledonian sulphide deposits and minor iron-formations from the southern Trondheim region, Norway.
(NGU (340), Journal article, 1978)Within the southern and central parts of the Trondheim region of the Norwegian Caledonides a great number of small, stratabound cupriferous pyrite deposits are confined to mafic metavolcanics of the Gula, Støren and Fundsjø ... -
Cier'te. Beskrivelse til det berggrunnsgeologiske kart 1733 II - 1:50 000 (med fargetrykt kart).
(NGU; Skrifter (331; 20), Journal article, 1977)A general description of the bedrock geology is presented. The map area has a threefold tectono-stratigraphic division. 1: The Precambrian (Sveco-karelian) besement rocks are subdivided into two complexes. The older one, ... -
Circum-Arctic Mapping Project - Gravity and magnetic maps (CAMP - GM)
(NGU-Rapport (2009.010), Report, 2010)An international effort to compile Circum-Arctic geophysical and bedrock data has been conducted by several national agencies (Russia, Sweden, Finland, Denmark, USA, Canada, Germany and Norway). This project produced an ... -
Contributions to the geology of the Mjøsa districts and the classical sparagmite area in Southern Norway.
(NGU (220), Journal article, 1963)This publication gives a survey of the main results of geological investigations carried out in the Mjøsa districts in central Southeast Norway by the author during recent years. The transitional situation of the districts ... -
Correlation between the Late Precambrian Older Sandstone series of the Varangerfjord and Tanafjord areas. Preliminary report.
(NGU (266), Journal article, 1970)Sedimentary rocks belonging to the late Precambrian Older Sandstone Series (overlain unconformably by the Eocambrian-Lower Cambrian Vestertana Group) are described from the Vadsø-Komagelva area on the northern side of ... -
Cu, Mo, Pb, Zn, Mn og Fe i bekkesedimenter, Finnemarka, Tyrifjord- området.
(NGU-Rapport (1650/49E), Report, 1979)1 137 bekkesedimenter ble prøvetatt med 250 m avstand i alle bekker. Prøvene ble analysert på Cu, Mo, Pb, Zn, Mn og Fe. Det ble påvist Mo-anomalier som sannsynligvis har sammenheng med den kjente Mo-forekomst ved Glitrevann. ... -
De fem jordartsregioner i Norge.
(NGU (195), Journal article, 1956)The five soil regions of Norway: The greater part of the deposits covering the rock in Norway were placed in their present position during the melting period of the inland ice. In studying the formation of soils two different ... -
De høymetamorfe bergartene øst for Røssvatnet: en feltrapport
(NGU-Rapport (98.137), Report, 1998)Denne rapporten presenterer foreløpige resultater av feltarbeid i området øst for Røssvatnet i Nordland, utført i perioden 9 juli - 10 september 1997. Arbeidet gjennomføres som et samarbeid med NGU og Institutt for geologi ... -
Deglasiasjonsforløpet i Aurlandsdalen og områdene omkring, Vest-Norge.
(NGU (317), Journal article, 1975)Ice movements and the course of deglatiation in the Aurland area are reconstructed. The oldest ice movement was from the SE-ESE and converged towards Aurlandsfjorden, while the younger movements were influenced by the local ... -
Den tillittførende formasjonsgruppe i Alta - en jevnføring med Øst-Finnmark og med indre Finnmark.
(NGU (228), Journal article, 1964)The Bosskop quartzite, the tillite layer and the succeedingbeds in Alta wer mapped by the present author in 1962. The mapping wasdone on aerial photographs at about 1:20 000. Fig. 1 give the result ona reduced scale. In ... -
Description of the geological maps "Tromsø" and "Målselv", Troms I. The Precambrian window of Mauken-Andsfjell.
(NGU (247), Journal article, 1967)This paper is the first part of a description of the bedrock on the two 1:100 000 map sheets, \"Målselv\" and \"Tromsø\". The geological map \"Målselv\", accompanies the paper. This part deals with the \"window\" of ... -
Det centrale Norges fjeldbygning
(NGU (39), Journal article, 1905)Forkortet: By Central Norway is here meant the three great valleys Østerdal, Gudbrandsdal and Valdres with their surroundings. In the district around lake Mjøsa there are opportunities for studying the differnt characteristics ... -
Detaljkartlegging av Grasbott skiferforekomst ved Notodden, Telemark
(NGU-Rapport (2002.115), Report, 2002)En kort befaring av Grasbott skiferforekomst i 2001 dannet grunnlaget for en mer detaljert undersøkelse i 2002. Undersøkelsen hadde som mål å kartlegge utbredelse av økonomisk drivbare partier av forekomsten. Arbeidet har ... -
Detaljkartlegging i Hessfjordområdet, Ringvassøy.
(NGU-Rapport (1800/14E), Report, 1980)Det er gjort en kartlegging og prøvetaking av mineraliseringene i gullfeltet på Ringvassøya. Gullfeltet ligger i et overskjøvet grønnsteinsbelte som antas å ha kaledonsk alder. Mineraliseringen er knyttet til kvartsganger ...