Blar i NGU Open Archive på emneord "KONGLOMERAT"
Viser treff 1-20 av 21
-
De eokambriske lag under hyolithussonen mellom Carajavrre og Caskias, Vestfinnmark.
(NGU (200), Journal article, 1957)In a previous note the author (Per Holmsen 1956, pp.- 65-72) has pointed out that the Eocambrian tillite occurs conformably below the basal beds of the \"Hyolithus-zone\" (lower Cambrian). During the summer1955 the ... -
Depositional environment and apparent age of the Fauske carbonate conglomerate, North Norwegian Caledonides.
(NGU Bulletin (436), Journal article, 2000)The Fauske conglomerate represents a rather rare case of a monomict carbonate conglomerate in the Late Neoproterozoic to Silurian, lithostratigraphic successions of the Norwegian Caledonides. Lithological varieties of this ... -
Forekomster av tillitt på nordsiden av Atnsjøvinduet, Syd-Norge.
(NGU (373), Journal article, 1982)A previously reported tillite-like conglomerate occurring on the northern side of the Atnsjø Window rests with an erosional contact on Precambrian granite and gabbro and is overthrust by fieldspathic metasandstones of the ... -
Fossils from pebbles in the Biskopåsen Formation in Southern Norway.
(NGU (251), Journal article, 1967)Fossils are reported from pebbles in the lowest part of the Biskopåsen Conglomerate in the Late Precambrian Lillehammer Subgroup at the norhtern end of lake Mjøsa in Southern Norway. The most common and widespread fossils ... -
Geologiske undersøkingar på Frøya og Froøyane.
(NGU-Rapport (90.073), Report, 1990)Kartlegging på Frøya og Froøyane har vist at berggrunnen for det meste er samansatt av kaledonske intrusivar som i nokre område innheld xenolittar av metasedimentere bergarter med ukjend alder. På Frøya og i ein del område ... -
Glacial stadials and interstadials of the Late Precambrian Smalfjord Tillite on Laksefjordvidda, Finnmark, North Norway.
(NGU (358), Journal article, 1980)Three glacial conglomerates and two intervening sandstones in the Smalfjord Formation on Laksefjordvidda were deposited during three glacial episodes and two interstadials, respectively. MOst of the sequence is preserved ... -
Grensen fyllitt - Valdres-sparagmitt i strøket sydøst for Grønsennknipa, Vestre Slidre.
(NGU (213), Journal article, 1961)In a paper of 1959 the writer described boundaries between the Ordovician \"phyllite formation\" and the overlying \"Valdres Sparagmite\" in and just east of the Grønsennknipa mountain mass, west of the Valdres valley, and ... -
Latest Precambrian and Eocambrian stratigraphy of Norway.
(NGU (251), Journal article, 1967) -
Microfossils from late Precambrian sediments around lake Mjøsa, Southern Norway.
(NGU (251), Journal article, 1967)Microfossils extracted with ordinary palynological methods from the Biskopås conglomerate (Biri-conglomerate) and the Biri-shale of the late Precambrian age in Southern Norway are described. Two principle categories of ... -
Naturstein i Solund
(NGU-Rapport (97.061), Report, 1997)I samarbeid med Solund kommune har NGU utført undersøkelser\/befaringer av fem blokksteinlokaliteter i kommunen. Undersøkelsene ble konsentrert om ulike varianter av konglomerat samt en grønnsteinsbreksje. Små blokk ble ... -
Noen iakttagelser fra Grønsennknipa i Vestre Slidre, Valdres.
(NGU (205), Journal article, 1959)In 1916 V.M. Goldschmidt published a well-known paper dealing with the conglomerates of the so-called \"Valdres Sparagmite\", a sedimentary series of mostly arkosic character which over large areas of the central part of ... -
Ordovician stratigraphy in the western Helgeland Nappe Complex in the Brønnøysund area, North-central Norway.
(NGU Bulletin (438), Journal article, 2001)In the western part of the Helgeland Nappe Complex, a small ophiolite fragment (the Bolvær Complex) and a metasedimentary succession (the Brønnøysund Group) are exposed on several islands to the west of Brønnøysund. The ... -
Rapport fra berggrunnskartlegging i Gjevingåsen for Nord-Trøndelag vegkontor
(NGU-Rapport (85.217), Report, 1985)Rapporten omfatter resultater fra berggrunnskartlegging av området mellom Hommelvik og Hell. Bergartene er beskrevet ut fra feltobservasjoner uten hensyn til den stratigrafiske gruppeinndelingen i Trondheimsfeltet, men med ... -
Skuringsmærker og morænegrus eftervist i Finmarken fra en periode meget ældre end "istiden"
(NGU (1), Journal article, 1891)Forkortet: The uppermost Fig. on p.79 shows the low mountains on the north side of the inner part of the Varangerfjord not far from the Russian border. At b and x occurs a little schist. The rest of the moountains consists ... -
Stratigraphy of the Sparagmite Group, including "the sandstone divisi- ons of Finnmark".
(NGU (208), Journal article, 1960) -
Studies on the latest precambrian and Eocambrian rocks in Norway
(NGU (251), Journal article, 1967) -
The stratigraphy of the Dyvikvågen Group, Stord : a revision.
(NGU (359), Journal article, 1980)A revision of the stratigraphy of the Upper Ordovician to Lower Silurian Dyvikvågen Group is presented. This group of sediments rests with primary stratigraphic unconfirmity upon a substrate of basaltic greenstones cut by ... -
The Ulriken Gneiss Complex and the Rundemanen Formation: a basement - cover relationship in the Bergen Arcs, West Norway.
(NGU Bulletin (412), Journal article, 1988)The Ulriken Gneiss Complex (UGC) and its sedimentary cover, the RundemanenFormation, have been investigated. The UGC is a Precambrian migmatite complexwhich suffered strong but heterogeneous reworking during the ... -
Undersøkelse av serpentinkonglomerat på Reiggehaugen, Vågå
(NGU-Rapport (2002.031), Report, 2002)Geologiske undersøkelser i forekomst av rødt serpentinkonglomerat ble utført i2001, og omfattet følgende:Geologisk overflatekartleggingSystematisk prøvetaking og fremstilling av slipte platerKjerneboring - tre vifter a tre ... -
Undersøkelse av Vadasbqak'ti serpentin/brucitt-forekomst i Lebesby kommune, Finnmark.
(NGU-Rapport (89.108), Report, 1991)En forekomst av skifrig serpentinitt med 15 % brucitt i store partier er undersøkt. Serpentinitten er 4,5 km lang, 2 km bred og har en mektighet opptil et par hundre meter. Brucitt er utviklet i skyvefronten ved den ...