Blar i NGU-publikasjoner på tittel
Viser treff 6033-6052 av 7138
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Storage potential for CO2 in the Beitstadfjord Basin, Mid-Norway
(NGU-Rapport (2004.036), Report, 2004)Forkortet The sedimentary sequence in the subsurface of the Beitstadfjord (Mid-Norway) has been assessed with regard to its suitablility for long-term storage of CO2. This study is part of the EU-funded CO2STORE project ... -
Storage potential for CO2 in the Froan Basin area of the Trøndelag Platform, Mid-Norway
(NGU-Rapport (2005.027), Report, 2005)Forkortet: The sedimentary sequence in the subsurface of the Trøndelag Platform (Mid-Norway) has been assessed with regard to its suitability for long-term storage of CO2. This study is part of the EU-funded CO2STORE project ... -
Storage potential for CO2 in the Frohavet Basin, Mid-Norway
(NGU-Rapport (2004.049), Report, 2004)The sedimentary succession in the subsurface of the Frohavet (Mid-Norway) has been assessed with regard to its suitability for long-term storage of CO2. This study is part of the EU-funded CO2STORE project and was stimulated ... -
Storisens transport av kisblokker fra Joma.
(NGU (203), Journal article, 1958)For three summers the Geological Survey of Norway has carried out a special hunt of pyrite boulders within the Grong area and adjacent districts. One result is the establishement of a marked boulder train from the Joma ... -
Storsjøreguleringen. Eventuell skade vannforsyning.
(NGU-Rapport (O-76056), Report, 1976)Vurdering av skade på vannforsyning som følge av Storsjøreguleringen. 3 brønner ble vurdert. Se også rapport av 1\/7-76. -
Storsjøreguleringen. Eventuelle tiltak vannforsyning Løsset.
(NGU-Rapport (O-76056-2), Report, 1976)Vurdering av tiltak for å utbedre vannforsyningen Løsset ved Storsjøen. Se også rapport av 3\/5- 76. -
Storskrymten 1418-1 kvartærgeologisk kart M 1:50 000
(Map, 2013) -
Storsteinnes. Kvartærgeologisk kart 1:15 000
(Map, 2007) -
Storvika, Nordreisa kommune. Kvartærgeologisk kart M 1:20 000
(Map, 2002)Vedlegg til NGU-.rapport 2001.120 -
Strandfladen, et nyt træk i Norges geografi
(NGU (14), Journal article, 1894)Forkortet: The western slopes of the Scandinavian peninsula do not generally extend quite to the sea; but we see there low almost level parts, which the author calls the Norwegian coast plain. The figures on pp. 1 and 2 ... -
Strandliniens beliggenhed under stenalderen i det sydøstlige Norge
(NGU (41), Journal article, 1905)Forkortet: Die Lage der Strandlinie w\u00E4hrend der verschieden Abschnitte der postglacialen Hebung. Zur L\u00F6sung dieser Aufgabe wurde eine Revision der fr\u00FCheren Untersuch- ungen \u00FCber die gleichzeitigen ... -
Strandlinjer og isavsmelting i midtre Hardanger, Vest-Norge.
(NGU (387), Journal article, 1983)In the Hardangerfjord area a shore-line diagram has been constructed on the basis of an earlier established shore-displacement diagram from Bømlo and 14C-dated marine levels from Stamnes, Bu and Eidfjord. Data from ... -
Strandlinjer, moræner og skjælforekomster i den sydlige del av Troms fylke
(NGU (94), Journal article, 1922)Within the Ofoten territory there are 5 good shore-lines as elsewhere in Northern Norway and besides these there is a 6th line farther to the north only observed near the heads of the fjords. These 6 lines have been measured ... -
Strategies for groundwater prospecting in hard rocks: a probabilistic approach
(NGU Bulletin (439), Journal article, 2002)Private wells in fractured, Precambrian, crystlline rocks are important for rural areas and small communities in Sweden. Since well yields normally are small, systematic approaches to groundwater prospecting are required ... -
Stratigraphical consequences of the discovery of Silurian fossils on Magerøy, the island of North Cape.
(NGU (247), Journal article, 1967)Crionid stems were discovered east of Norvågen (east of Honningsvåg) on Magerøy in 1939. In 1960 an additional find of fossils proved a Silurian age for the limestone and conglomerate beds there. Two years later the athor ... -
Stratigraphical position of the Gudå conglomerate zone.
(NGU (227), Journal article, 1964)The Gudå conglomerate zone has been considered to be of Upper Ordovician to Lower Silurian age. The main argument for this conclusion has been that the conglomerates of this zone have been the same pebble composition as ...