NGU-publikasjoner: Nye registreringer
Viser treff 341-360 av 7138
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Grunnvann øst for Oslo-feltet. Meddelelse fra Vannboringsarkivet nr. 10.
(NGU (213), Journal article, 1961)A rapid survey of the general geology south, east and northeast of Oslo is given with a view to explain the differences in water supply in various Precambrian rocks. The gneisses usually give much more water than the more ... -
Groundwater transit times in a small coastal aquifer at Esebotn, Sogn og Fjordane, western Norway
(NGU Bulletin (431), Journal article, 1996)A shallow alluvial aquifer in Esebotn, Sogn og Fjordane, Norway has been investigated from a hydrological standpoint in order to obtain estimates of groundwater transit times. Water levels, oxygen isotopes, water temperatures ... -
Orienterende undersøkelser vedrørende sprøhet og flisighet av bergarter.
(NGU (247), Journal article, 1967) -
Studies on the Latest Precambrian and Eocambrian Rocks in Norway
(NGU (238), Journal article, 1966) -
Fossilførende sedimenter ved Skudenes.
(NGU (155), Journal article, 1940)The southern part of the island Karmøy (Western Norway, between Stavanger and Haugesund) displays a varying complex of slightly metamorphic sediments and igneous rocks: besides gabbro, there occur conglomerates, \"fragmental ... -
A beryllium-magnetite correlation in the Hørtekollen-Grubeås area, Buskerud, Norway, and its use for beryllium prospection.
(NGU (223), Journal article, 1963)A helvite-magnetite mineralization at Hørtekollen was studied for its beryllium and magnetite contents. Statistically, a close correlation between the magnetite and the beryllium contents was found to occur. Therefore a ... -
Om oversiluren i Brumunddalen
(NGU (37), Journal article, 1903)The Brumunddal (dal means valley) lies in the middle part of Southern Norway and ascends from the lake of Mjøsa to the North of the town of Hamar. Silurian shales and limestone, postsilurian porphyry and a sandstone occur ... -
Bemærkninger om oversiluren i Brumunddalen
(NGU (37), Journal article, 1904)Forkortet: The author can not agree in some points of the description of the Upper Silurian in Brumunddalen, which Mr.K.O.Bjørlykke has published in \"Norges geologiske undersøkelses Årbok\" (1904 No.2). I. The graptolitic ... -
Change in chemical composition of rock samples during preparation for analysis.
(NGU (300), Journal article, 1973)It has been shown that up to 3% of the volume of rock samples may escape as clust during their preparation (crushing and grinding) for chemical analysis. The mineral and chemical composition of the escaping rock dust may ... -
Grunnvann. Kunstig infiltrasjon. GiN-veileder nr. 11
(Skrifter (109), Journal article, 1992) -
Isavsmelting i og omkring midtre Gudbrandsdalen.
(NGU (223), Journal article, 1963)Observed glacial striae showing direction of ice-movement during the last active stage of the inland-ice are shown in fig. 1. Supposed major directions of ice movement are also shown in fig. 3. In the mountain parts are ... -
The Ordovician Grøndalsfjell Intrusive Complex: Central Scandinavian Caledonides: field relations, petrography and emplacement
(NGU Bulletin (435), Journal article, 1999)The Grøndalsfjell Intrusive Complex (GIC) is part of a major plutonic province located in the Gjersvik Nappe of the Upper Allochthon in the Caledonides of Central Norway. Field relationships and petrography suggest that ... -
Dunderlandsdalen. Fjeldbygningen inden gradavdelingskartet Dunderlandsdalens omraade
(NGU (86), Journal article, 1919)This paper is a geological description of the Dunderland district in Nordland, a part of Northern Norway. The map accompanying the paper is a part of the official series of maps on the scale of 1:100 000, which is being ... -
Baseflow production from partially peat-covered catchments, Jonsvatnet, Mid-Norway
(NGU Bulletin (422), Journal article, 1992)Forkortet: To their wide areal extent and high water release capability, peatland ecosystems must have a significant, albeit hitherto poorly quantified, influence on baseflow production in partially peatcovered catchments. ... -
Geological and petrographical investigations in the Kongsberg-Bamble formation.
(NGU (160), Journal article, 1943)The rocks of the Kongsberg-Bamble Formation are Pre-Cambrian and belong to the deeper parts of an ancient mountain range (the Sveco-Fennides). The main geological features appear from Table 11. In comparison with the ... -
Natural stone in Norway: production, deposits and development
(NGU Bulletin (436), Journal article, 2000)The natural stone industry has, during the last two decades, experienced a tremendous growth both on a global scale and within a Norwegian context. At the present time, the natural stone industry contributes significantly ... -
Iakttagelser fra Rektangelbladet Kragerø og Den store Grunnfjellsbreksje.
(NGU (229), Journal article, 1965) -
The deglaciation of the coastal area NW of Svartisen, northern Norway.
(NGU (369), Journal article, 1981)Late Weichselian glacial events, marine fauna and shore-lines in the coastalarea NW of Svartisen are described. During the oldest glacial event (Vassalevent), marginal moraines were deposited near the mouths of the fjords. ... -
Age determination from the Trondheim Region Caledonides, Norway: a preliminary report.
(NGU (288), Journal article, 1973)Twenty-four potassium-argon age determinations have been made on metamorphic minerals and whole-rocks (phyllites) from the Caledonides of the Trondheim region, Norway. Nineteen of the apparent ages fall between 438 and 402 ... -
Kort beskrivelse av bergartene.
(NGU Bulletin (155), Journal article, 1940)Petrographic inspection of the rocks reveals that all of them, both sedimentary and igneous, are metamorphic. The igneous rocks are gabbroic and trondhjemitic. The rocks of gabbroic origin (among them probably hypabyssal ...