Content type

Publication type

Publication series

Downloadable

Year published

County

9668 results
All available information on the most important metal- and diamond deposits in the Arctic has been assembled in a book (accompanied by a map) and in a database.
Norges geologiske undersøkelse har på oppdrag for Statens Vegvesen gjort en vurdering av en skiferforekomst i Snilldal i Snillfjord kommune. Ny fylkesvei 714, Laksevegen, gjennom Snilldalen ble åpnet i 2017. Den nye veien går ved Kudalen/Antonrommet ca 30 meter lenger mot nordøst enn tidligere og skjærer der gjennom sone med skifrig kvartssandstein; registret som en skiferforekomst i NGU’s natursteinsdatabase. Forekomsten ble befart 10.
Rapporten inneholder resultater fra geofysiske målinger fra helikopter over et område mellom Innerdalen og Igelfjell i syd og nord samt Berkåk og Nerskogan i øst og vest. Området er i denne rapporten kalt Oppdal. Det ble fløyet 3 100 profilkilometer med 200 meter profilavstand og dette dekket ca. 620 km2. Rapporten inneholder dessuten data fra noen ekstra profiler fløyet for NGU utenfor den sydvestlige delen av området ved Skarvatnet.
The Ramså Basin in the northeast of the island of Andøya combines both a Mesozoic sedimentary succession and a subjacent deeply weathered basement. The basin must be considered as the only easily accessible analogue for the setting and development of the offshore Mesozoic basins.
The Geological Survey of Norway (NGU) has previously been in involved in two reports describing the geological conditions along the trace of the ROGFAST tunnel. There it was concluded that the geological information for the area between Kvitsøy and Bokn was too scattered to give a reliable interpretation of the geology.
Ti sedimentprøver fra norske havområder er analysert for innhold av mikroplast. Prøvene er fra forskjellige avsetningsmiljøer, og analysene er utført på åtte sedimentkjerner tatt med multicorer og to prøver tatt med bokscorer. De øverste 3 cm med sediment på havbunnen er tatt ut for å ekstrahere og analysere mikroplast. Prøvene ble sendt til et laboratorium i Belgia for opparbeiding og analyse av mikroplast.
NGU utførte i årene 2005-2006 og 2009-2010 georadarmålinger og refraksjonsseismikk i Bødalen i forbindelse med løsmassegeologisk forskning i Stryn kommune i Sogn og Fjordane fylke. Målingene er utført både i øvre del av dalføret, dvs. i området like foran brefronten av Bødalsbreen og ved Bødalssetra nordafor, og dessuten på elvedeltaet i Lovatnet nederst i dalen mot V.
The Jan Mayen microcontinent is a small, unique, crustal entity that was separated from the Norwegian and Greenland margins by two distinct rifting events. Seafloor spreading along the Aegir Ridge separated Jan Mayen (together with Greenland) from Norway by ca. 54 Ma. Cessation of seafloor spreading on the Aegir Ridge at ca. 30 Ma was more or less simultaneous with the onset of extension along the Kolbeinsey Ridge between Jan Mayen and Greenland. Break-up along the Kolbeinsey Ridge by ca.
This report presents maps of sedimentary environments and seabed sediments (genesis) in the Nordland VI management area off northern Norway. The maps, which cover about 25 000 km² and water depths from 60 m to 2700 m, are based on multibeam echosounder data (bathymetry and backscatter), 215 video lines each 700 m long, seabed sediment samples from 40 stations (grab, boxcore and multicore) and 5500 km of sub-bottom profiler data.
NGU utførte i 2007 georadarmålinger i Troms i forbindelse med løsmasseundersøkelser ved to lokaliteter ved Skibotn i Storfjord kommune og ved lokalitetene Brandmoen og Mortenelva i Målselv kommune. Målingene omfatter totalt 8 profiler med samlet lengde 4703 m.
As a part of the MINN project (Minerals in Northern Norway) a helicopter-borne geophysical survey were performed at Senja in 2012 – 2014. Electromagnetic data from this survey showed up anomalies that could be caused by large graphite mineralisations. Geophysical and geological follow-up work was carried out at three locations in 2016, Hesten, Vardfjellet and Grunnvåg, with additional funds from the Troms County administration.
The landscape story told on this map is the result of geology, geomorphology and climate driven processes in high arctic Svalbard. The map informs about the landscape we see today and also gives information about hazards and challenges we face when traveling in it.
Fordelingen av løsmasser og landskapsformer forteller om de dannelsesprosesser som skjer og har skjedd tidligere i landskapet, og kartet er nyttig for å forstå endringer i miljøet over tid, og hva en bør tenke på ved ferdsel gjennom landskapet.
Middle and Late Pleistocene stratigraphy, chronology and glacial history in Finnmark, North Norway.Lars Olsen, Vagn Mejdahl, Synøve F.
Caledonian structural evolution and tectonostratigraphy in the Rombak - Sjangeli Window and its covering sequences, northern Scandinavian CaledonidesGerhard BaxPage(s): 87-104
Subduction-related volcanism in the Gula Nappe, southeastern Trondheim Nappe Complex, Central NorwayElizabeth A.
Neotectonics in the Ranafjorden area, northern NorwayOdleiv Olesen, Svein Gjelle, Herbert Henkel, Tor Arne Karlsen, Lars Olsen, Terje SkogsethPage(s): 5-8
Tectonometamorphic evolution of the allochthonous caledonian rocks between Malangen and Balsfjord, Troms, North norwaySteffen G.
Distribution of rock fragments, grain size and chemical elements of tills in the Lake Mjøsa area, eastern NorwayBjørn A.
A buried late MIS 3 shoreline in northern Norway - implications for ice extent and volumeLars OlsenPage(s): 1-14Download
Groundwater transit times in a small coastal aquifer at Esebotn, Sogn og Fjordane, western NorwayHelge Henriksen, Noralf Rye, Oddmund SoldalPage(s): 5-17
Field relations and geochemical evolution of the Gothian rocks in the Kvamsøy area, southern Western Gneiss Complex, NorwayØyvind SkårPage(s): 5-23
Upper Cambrian and lower Tremadoc olenid trilobites from the Digermul peninsula, Finnmark, northern Norway.Frank NikolaisenPage(s): 1-49Coastal caves and their relation to early postglacial shore levels
Groundwater contribution to a mountain stream channel, Hedmark, NorwaySylvi Haldorsen, Jens-Olaf Englund, Per Jørgensen, Lars A.
Radiocarbon dates from the mountain area northeast of Årdal, southern Norway, evidence for a Preboreal deglaciation.Atle Nesje, Noralf RyePage(s): 1-7
Glacial geology of Middle and Inner Nordfjord, western Norway.Olav W. FarethPage(s): 1-55
New data on Upper Ordovician conodonts from theTrondheim Region, Central Norwegian CaledonidesT.
Timing of late- to post-tectonic Sveconorwegian granitic magmatism in South Norway.Tom Andersen, Arild Andresen, Arthur G.
Primary and re-equilibrated mineral assemblages from the Sveconorwegian mafic intrusions of the Kongsberg and Bamble areas, Norway.John D. Brickwood, James W.
Geology and structural evolution of the Precambrian rocks of the Oslofjord - Øyeren area, Southeast Norway.Ole GraversenPage(s): 1-50 + ka
The conglomerates of the Sel Group, Otta-Vågå area, Central Norway: an example of a terrrane-linking successionR. Bøe, B.A. Sturt, D.M.
Aeromagnetic and gravimetric interpretation of regional structural features in the Caledonides of West Finnmark and North Troms, Northern Norway.Odleiv Olesen, David Roberts, Herbert Henkel, Ole Bernt Lile, Trond H.
Tectonostratigraphy and tectonic evolution of the Skånland area, North Norway.Mark G.
High-temperature ultramafic complexes in the North Norwegian Caledonides: I - Regional setting and field relationships.M.C. Bennett, S.R. Emblin, B.
Geological note: Petrophysical and thermal properties of pre-Devonian basement rocks on the Norwegian continental marginTrond Slagstad, Cécile Barrére, Børre Davidsen, Randi K.
Regional geophysics of the Central Norwegian Caledonides.Fredrik Chr. WolffPage(s): 1-27Determination of density of rocks: a comparison of various methods of calculation.Fredrik Chr.
Tectonostratigraphy in the Velfjord-Tosen region, southwestern part of the Helgeland Nappe Complex, Central Norwegian Caledonides.Terje Thorsnes, Helge LøsethSide(r): 1-18
Late Proterozoic (Vendian) to Early Cambrian sedimentation in the Hedmark Group, south-western part of the Sparagmite Region, southern NorwayTom DreyerPage(s): 1-27
Sedimentology of the Upper Proterozoic glacial record, Vestertana Group, Finnmark, North Norway.Marc B. EdwardsPage(s): 1-76

Pages