NGU-publikasjoner: Recent submissions
Now showing items 561-580 of 7138
-
Praktisk-geologiske undersøgelser af Nordlands amt. I. Salten og Ranen med særlig hensyn til de viktigste jernmalm- og svovelkis-kobberkis- forekomster samt marmorlag
(NGU (3), Journal article, 1890)Forkortet: Die vorliegende Abhandlung erscheint als erster Theil einer geologischen Bescreibung von Nordland Amt, mit besonderer R\u00FCcksicht auf die wichtigsten Marmorlager und Erzlagerst\u00E4tten (von Eisenerz, ... -
Bergartsklassifikasjon og kartsammenstilling. Klassifikasjon av bergarter. Rettledning for forfattere av berggrunnskart. Norsk-engelsk og engelsk-norsk ordliste.
(Skrifter (113), Journal article, 1995) -
Geothermal aspects of hydrocarbon exploration in the North Sea area.
(NGU (316), Journal article, 1975) -
Norges Geologiske Undersøkelse. Årsberetning for 1958
(NGU (205), Journal article, 1959) -
Aarbog for 1892 og 93
(NGU (14), Journal article, 1894)Strandflaten, et nyt træk i Norges geografi av Hans Reusch. Mellem Bygdin og Bang av Hans Reusch. Har der existeret store, isdæmmede indsjøer paa østsiden av Langfjeldene av Hans Reusch. Høifjeldskvartsens nordøstligste ... -
The Eidsfjord anorthosite, Vesterålen, Norway: field observations and geochemical data.
(NGU Bulletin (434), Journal article, 1998)New fieldwork in the Eidsfjord anorthosite on Langøy, Vesterålen, Nordland, has revealed that the anorthosite in the centre of the investigated complex is associated with large amounts of monzonitic and more mafic rocks ... -
Notes on the geology of an area west of Støren (the Trondheim region).
(NGU (223), Journal article, 1963)In the paper a brief survey of the stratigraphy and structure of the Ordovician-Silurian sedimentary complexes in the western surroundings of Støren (the Trondheim region) is presented and some results of Prof. Th. Vogt's ... -
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 ... -
Structural evolution of the Bergsdalen Nappes, Southwest Norway
(NGU Bulletin (424), Journal article, 1993)The Bergsdalen nappes are Caledonian thrust sheets which experienced perva- sive, although heterogeneous ductile deformation during the upper green- schist to lowermost amphibolite-facies, Caledonian, thrusting history. ... -
Regional similarities in the distribution of well yield from crystalline rocks in Fennoscandia
(NGU Bulletin (450), Journal article, 2010)Well yields from Precambrian and Palaeozoic bedrock in Norway, Sweden and Finland exhibit very similar and approximately log-normal distributions: all three data sets exhibit a median yield of 600-700 L hr-1, despite the ... -
Fotogeologi
(NGU (205), Journal article, 1959)The use of air photos for geological interpretation is described. A short introduction to photogrammetry is given, and the types of instruments useful for photogeology are mentioned. -
Røros. Beskrivelse til kvartærgeologisk landgeneralkart
(NGU (198), Journal article, 1956)The present map, dealing with the quarternary deposits of Røros, is partly based on existing maps of a larger scale, certain of which have been published. Areas not geologically mapped beforehand were surveyed in the susal ... -
Melt-mineral-fluid interaction in pealkaline silicic intrusions in the Oslo Rift, Southeast Norway. II. High temperature fluid inclusions in the Eikeren-Skrim.
(NGU Bulletin (417), Journal article, 1990)The Eikeren-Skrim subvolcanic granite complex consists of mildly peralkaline rocks, most of which contain abundant miarolitic cavities. Optical microscope studies reveal that several generations of fluids and solids were ... -
Det nordvestlige gneis-område i det sydlige Norge, aldersforhold og tektonisk-stratigrafisk stilling.
(NGU (184), Journal article, 1953) -
Geologisk kart med beskrivelse over Kristiania by
(NGU (25), Journal article, 1898)Forkortet: The present treatise is a description of the geological map of Oslo, a tack which was prescribed in 1893-94 by the authorities of the Academic College of the University in competition for the gold medal awarded ... -
Chemical and petrographic characterization of ilmenite and magnetite in oxide-rich cumulates of the Sokndale Region, Rogaland, Norway
(NGU Bulletin (436), Journal article, 2000)Igneous ilmenite and magnetite in some oxide-rich cumulates of the Sokndal region show chemical features and microtextures that reflect the progress of magmatic evolution and subsolidus re-equilibration. These features ... -
An example of granitization in the central zone of the Caledonides of Northern Norway. Et eksempel på granittisering i den sentrale sonen av Kaledonidene i Nord-Norge.
(NGU (184), Journal article, 1953)A brief outline of the geology of the Holandsfjord area is given and the structural evolution and the granitization processes are discussed. It is concluded that the large masses of granite overlying the paragneisses may ... -
Geology and structural evolution of the Precambrian rocks of the Oslofjord - Øyeren area, Southeast Norway.
(NGU Bulletin (398), Journal article, 1984)The area (1200 km\u00B2) described covers the northern part of a major thrust segment in the eastern subprovince of the Sveonorwegian orogenic belt along the southwestern margin of the Baltic Shield. The oldest rock unit ... -
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 ... -
Utgliding av jernbanefylling ved Kolbotn stasjon.
(NGU (166), Journal article, 1946)This station lies on the Østfold railway, 13 km from Oslo. One day in November 1936 a 4 m high newly built ballast with the rails on it suddenly sunk into a ground consisting of peat and a weak clayey deposit. Over a ...