Browsing NGU Open Archive by Title
Now showing items 6209-6228 of 7131
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TFEM-målinger, Gjersvikklumpen, Røyrvik, Nord-Trøndelag
(NGU-Rapport (95.004), Report, 1995)Det er gjort TEFM-målinger (Tids- og Frekvensdomenet ElektroMagnetiske målinger) i et 8 km\u00B2 stort område over Gjersvikklumpen. Hensikten var å undersøke om dype massive sulfidmalmer kunne indikeres. Geologiske ... -
TFEM-målinger, Tunnsjøflyin, Namsskogan, Nord-Trøndelag
(NGU-Rapport (95.125), Report, 1995)Det er gjort TFEM-målinger (Tids- og Frekvensdomenet ElektroMagnetiske målinger i et 2 km\u00B2 stort område ved Tunnsjøflyin. Hensikten var å undersøkes utbredel- sen av en tidligere kjent sulfidmineralisering og om ... -
The "Better to burn out than to fade away" tour: magma-driven, high-grade metamorphism in the Sveconorwegian Province, SW Norway during the terminal stages of Fennoscandian Shield evolution. NGF/NPF field-trip guide, 11. June 2017
(NGU-Rapport (2017.030), Report, 2017)The exposed rocks in Rogaland, that we will study on this field trip, provide insight into processes in the lower and middle crust of a long-lived, late Mesoproterozoic continental-margin arc, on tens of million year time scales. -
The 5th seminar on hydrogeology and enviornmental geochemistry - "B.Bølviken Seminar -95"
(NGU-Rapport (95.138), Report, 1995)The 5th seminar on Hydrogeology and Environmental geochemistry \"B.Bølviken Seminar -95\" was arranged on Nov.9.and 10.1995 in Trondheim. The lectures dealt with the three main topics: Groundwater as a resource, Hydrogeochemistry ... -
The 6th Seminar on Hydrogeology and Environmental Geochemistry 1996
(NGU-Rapport (96.128), Report, 1996)The 6th seminar on Hydrogeology and Environmental Geochemistry was arranged on nov. 11. and 12. 1996 at the Knut S.Heier Conference Centre. NGU, Trondheim. The first day was primarily used for discussions of hydrogeological ... -
The Agip NSD-1 well at Tananger
(NGU-Rapport (97.176), Report, 1997)Geological description of well logs, cuttings and surface samples in the Tananger-Sandnes area was carried out in order to gain a wider understanding of the Caledonian nappe sequences. The upper part of the Jæren Nappe ... -
The Alice Wain Memorial West Norway Eclogite Field Symposium, abstract volume
(NGU-Rapport (2003.055), Report, 2003)This report contains the scientific program and abstract volume for the lectures and posters presented during the Alice Wain Memorial West Norway Eclogite Field Symposium. The lecture and field symposium, held in Selje ... -
The alkaline complex of the Breivikbotn area, Sørøy, Northern Norway.
(NGU (231), Journal article, 1965)The alkaline rocks of the Breivikbotn area have been emplaced into highly folded and metamorphosed igneous and sedimentary rocks during the period of the Caledonian orogeny. They form an integral part of the complicated ... -
The Archaean-Proterozoic boundary beneath the Caledonides of northern Norway and Sweden: U-Pb, Rb-Sr, and isotope data from the Rombak-Tysfjord
(NGU-Rapport (91.225), Report, 1992)The Baltic Shield includes an Archaean craton in northeastern Finland. Early Proterozoic accretions to this Archaean craton comprise of (1) the Svecofen- nian domain, which consists of island arc volcanic and sedimentary ... -
The basal gneisses and basement contact of the Hestbrepiggen area, North Jotunheimen, Norway.
(NGU (252), Journal article, 1968)Pethographic, modal, chemical, X-ray and structural studies have been made on rocks from a mapped area of Basal Gneisses and Basement contact in a glaciated region in the North Jotunheim mountains. Precambrian Basal Gneisses ... -
The bedrock geology of Varanger Peninsula. Excursion Guide.
(NGU-Rapport (90.082), Report, 1990)Kartblandnr. og -navn (M.1:50 000) forts.: 2335 I-IV, 2435 I-IV, 2436 III-IV, 2536 IV. The Varanger Peninsula is underlain by weakly metamorphosed sedimentary rocks of Late Precambrian to Early Cambrian age. The rocks occur ... -
The Björkö geothermal energy project
(NGU Bulletin (439), Journal article, 2002)Impact crater formation results in changes in the physical properties of rocks that can be geophysically determined and therefore are of importance for the mapping structures at depth. Especially electrical properties have ... -
The Bleikvassli Project, field report 1997
(NGU-Rapport (98.074), Report, 1998)This report presents preliminary results of detailed geological follow-up studies and diamond drilling carried out in the Okstindan Area, Nordland, Norway in the period July to August 1997. Preliminary results from drilling ... -
The Bordvedåga beryllium deposit, Rana, Nordland County, Norway. Summary report.
(NGU-Rapport (91.181), Report, 1991)Investigations in the Høgtuva and Sjona basement windows in Nordland County were carried out from 1980 to 1990. Detailed work including drilling on the Be-deposit at Bordvedåga was done from 1984 to 1988 by NGU in cooperation ... -
The Caledonian Basement. Reply to Per Holmsen.
(NGU (234), Journal article, 1965) -
The Caledonian fold belt i Finnmark
(NGU Bulletin (403), Journal article, 1985)Forkortet. The Caledonian allochthon in Finnmark embraces 4 major nappes or nappe complexes named, from bottom to top, the Gaissa, Laksefjord, Kalak and Magerøy. Of these the 3 lower nappe complexes acquired their internal ... -
The Caledonian mountain chain of the Southern Troms and Ofoten areas. Part I. Basement rocks and Caledonain meta-sediments.
(NGU (239), Journal article, 1966)The geology of the present area will be treated in a series ofthree publications. In the first paper the petrography and generalfeatures of the Precambrian rocks and the so-called \"basal gneisses\"are described and the ... -
The Caledonian Mountain Chain of the Southern Troms and Ofoten areas. Part II. Caledonian rocks of igneous origin.
(NGU (261), Journal article, 1969)Metamorphosed rocks of igneous origin are described fromCaledonian part of the Southern Troms and Ofoten areas. Based onmegascopic and microscopic appearance, on chemistry and on fieldrelations they can be divided into two ... -
The Caledonian mountain chain of the Southern Troms and Ofoten areas. Part III. Structures and structural history.
(NGU (283), Journal article, 1972)The main lines of the structural geology of the area of about 13,000 km\u00B2 in the Caledonian mountain chain of Northern Norway are described. The major structure is characterized by nappes with a thrust front in the ... -
The Caravarri Formation of the Kaukokeino Greenstone Belt, Finnmark, North Norway: a Palaeoproterozoic foreland basin succession.
(NGU Bulletin (442), Journal article, 2004)The Caravarri Formation is the youngest supracrustal unit in the Palaeoproterozoic Kautokeino Greenstone Belt of western Finnmark. This greenstone belt and correlative units at Alta farther north were formerly ascribed to ...