Browsing NGU Open Archive by Title
Now showing items 7041-7060 of 7131
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Weichselian and Holocene geology of Sør-Trøndelag and adjacent parts of Nord-Trøndelag county, Central Norway
(NGU Bulletin (426), Journal article, 1994)In Sør-Trøndelag and adjacent parts of Nord-Trøndelag a clayey till (10-25% in the clay fraction) is commonly found below 1-5 m of sandy till (1-5% in the clay fraction). The clayey till is mostly found in drumlins, in ... -
Weichselian ice movements, sediments and stratigraphy on Hardanger- vidda, South Norway.
(NGU (350), Journal article, 1979)Based on studies of glacial directional elements and on lithology, palynology and stratigraphy of the Quaternary sediments, the following climatostratigraphy and ice movement patterns are indicated; an early ice-free period, ... -
Western European Geological Surveys (WEGS), Working Group on Regional Geochemical Mapping. Project Proposal.
(NGU-Rapport (88.147), Report, 1988)It is proposed to perform an orientation survey in three parts (1) complete an inventory of the regional geochemical mapping thus far done in all WEGS countries (1988-89), (2) collect overbank sediments at various depths ... -
Wolfram i Salten-regionen. Statusrapport.
(NGU-Rapport (87.177), Report, 1987)Med økonomisk støtte fra NGUs USB-prosjekt har en gruppe fra København Universitet under ledelse av lektor Henrik Stendal, utført metallogenetiske undersøkelser av W-mineraliseringer i Salten-regionen. I øyeblikket pågår ... -
Wolfram og platinaundersøkelser i Skjerstad kommune, Nordland.
(NGU-Rapport (88.179), Report, 1988)Wolfram er påvist i anomale mengder ved Hoset. Analyser av bekkesedimenter gir verdier opptil 1.1% WO3. Wolfram er knyttet til mineralet schelitt, som er fun net i forbindelse med to typer skarnmineraliseringer - diopsidskarn ... -
Wolframmineraliseringer i Bodø-Glomfjord-regionen
(NGU-Rapport (92.231), Report, 1993)Bodø-Glomfjord-regionen inneholder et betydelig antall wolfram-(scheelitt) mineraliseringer. Scheelitt opptrer disseminert i karbonatholdige glimmerskifre i turmalinitter, på kvartsganger, pegmatitter og i skarnmineraliseringer. ... -
Wolframprospektering II i Grongfeltet, Nord-Trøndelag.
(NGU-Rapport (1316), Report, 1974) -
Wollastonittundersøkelser i Nordland
(NGU-Rapport (94.016), Report, 1994)I Nordland fylke utgjør lag av kalkspatmarmor en markert andel av det geologiske kartbildet. Kontaktmetamorfose i tilknytning til de mange intrusiver om opptrer sammen med kalkene tilsa at mulighetene for wollastonittdannelse ... -
World-wide 2 billion-year-old isotopically heavy carbonate carbon: the evolutionary significance and driving forces (final report).
(NGU-Rapport (99.103), Report, 1999)This report shows the activities carried out and the results obtained within the project. The results shown in this report have been obtained within period of time from 30.11.96 to 15.09.99. -
World-wide 2 billion-year-old isotopically heavy carbonate carbon: the evolutionary significance and driving forces. Annual report
(NGU-Rapport (97.171), Report, 1997)This report will show the activities carried out and the results obtained within the project entitled \"World-wide 2 billion-year-old isotopically heavy carbonate carbon: the evolutionary significance and driving forces\". ... -
XRD bestemmelse av fiber i Åheim dunitt
(NGU-Rapport (2002.026), Report, 2002)I en tilsendt prøve av borkaks, med mye fiber fra Gusdalsbruddet ble det ved bruk av røntgendiffraksjon (XRD) påvist opptreden av amfibolen antofyllitt. Dette er en Ca-fattig, Mg- og Fe-rik rombisk amfibol. For å teste XRD ... -
Young Trondhjemites 2017 – Programme and Abstracts
(NGU-Rapport (2017.028), Report, 2017)Young Trondhjemites 2017 is the second edition of a conference for young researchers working with geosciences and engineering in Trondheim. The conference was held the 2nd of June at the Geological Survey of Norway (NGU) ... -
Young Trondhjemites 2018 - Program and abstracts
(NGU-Rapport (2018.006), Report, 2018)Young Trondhjemites, the conference for young researchers working with geosciences and engineering in Trondheim, has been arranged in 2018 for the third time. The conference has been held at the Geological Survey of Norway ... -
Young Trondhjemites 2019 - Program and abstracts
(NGU-Rapport (2019.011), Report, 2019)The 4th Young Trondhjemites conference for young researchers working in geoscience and geological engineering was held at NGU on 22nd March 2019.The young researcher community contributed with 11 oral presentations and 9 ... -
Ytre Rendal og Stor-Elvdal. Beskrivelse til de geologiske rektangel- kart.
(NGU (194), Journal article, 1956)The solid rocks of the map sheet Ytre Rendal and Stor-Elvdal have been mapped by per Holmsen and Chr. Oftedahl. The rock types belong to the following groups: Precambrian, essentially granitic rocks. Sparagmite Group, ... -
Zinc and lead deposits in the Håfjell syncline, Ofoten, northern Norway.
(NGU (244), Journal article, 1967)This paper deals with the stratigraphic position, the tectonic development and the major mineralogy of the ores and imediate wall rocks of the Håfjell syncline, on the southern side of the Ofoten fjord, Northern Norway. ... -
Zn-Pb forekomstene på Nonsfjellet og Vassheia, Beiarn kommune, Nordland
(NGU-Rapport (2003.085), Report, 2003)Forekomstene på Nonsfjellet og Vassheia har vært kjent i 125 år og har vært undersøkt i flere perioder. Det er drevet noen korte synker for å undersøke forekomstene. De er sink-bly (Zn-Pb) forekomster med et lavt kobberinnhold ... -
Zur Geologie und Tektonik des Akersvatn Gebietes, Rana, Nordland.
(NGU (327), Journal article, 1976)The Akersvatn region is located within the high-metamorphic R\u00CEdingsfj\u00CCll Nappe in the Central Scandinavian Caledonides. The investigated area is subdivided into three tectonic units: The Græsfjell Complex, the ... -
Zur Petrographie des Valdres-Sparagmites zwischen Bitihorn und Langsuen/Valdres (Süd-Norwegen).
(NGU (243B), Journal article, 1967)Der Valdres-Sparagmite zwischen Bitihorn und Langsuen zeigtfolgende Ausbildungsarten: 1. Langsu-Formation (400 m) a)Muskovit-Epidot-Aktinolith-Schiefer mit klastischen Hornblende, b)Plagioklas- und epidotreiche Sparagmite ...