Browsing Artikler by Title
Now showing items 464-483 of 1064
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Labrador
(NGU (1), Journal article, 1891)Forkortet: Labrador. This is the name in trade for the beautiful dark grey augite-syenite with labradorizing soda-orthoclase from the region of Frediksværn and Larvik on our Southcoast. -
Lagfølgen på Hardangervidda og den såkaldte "høifjeldskvarts"
(NGU (11), Journal article, 1893)Forkortet: Der Alaunschiefer ist namentlich in s\u00FCd\u00F6stlichsten Theil von Vidda typisch ausgebildet; die Schiefer sind nicht mehr unver\u00E4nderte Alaunschiefer sondern regionalmetamorphische Aequivalente. Zu ... -
Large continental rotations during Vendian and Palaeozoic times: a simple geodynamic explanation
(NGU Bulletin (427), Journal article, 1995)Frie emneord: Platerotasjon -
Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark.
(NGU (269), Journal article, 1971)The presence of two closely spaced tillite formations within the Precambrian and Cambro-Ordovician sediments of eastern Finnmark permits subdivision into pre-glacial and post-glacial regimes. On the northern side of ... -
Late Precambrian sedimentary rocks of the Tanafjord-Varangerfjord region of Varanger peninsula, Northern Norway.
(NGU (269), Journal article, 1971)The late Precambrian Older Sandstone Series of Føyn (1937) underlies relatively large areas od the Tanafjord-Varangerfjord region of Varanger Peninsula (Siedlecka & Siedlecki, 1967). Geological mapping carried out by the ... -
Late Precambrian stratigraphy and structure of the north-eastern margin of the Fennoscandian shield (East-Finnmark - Timan Region).
(NGU (316), Journal article, 1975)Later Precambrian (Riphean and Vendian) rocks occur along the north-easternb margin of the Fennoscandian Shield and the Russian Platform in Three zones: 1) the Varanger-Kildin, 2) the Timan-Kanin and 3) the Southern Barents ... -
Late Proterozoic (Vendian) to Early Cambrian sedimentation in the Hedmark Group, south-western part of the Sparagmite Region, southern Norway
(NGU Bulletin (412), Journal article, 1988)Field studies of the allochthonous Ekre Shale and Vangsås Formation (uppermost Hedmark Group) were undertaken in order to develop a sedimentary model for the final stages of infilling of the Hedmark rift basin. The Ekre ... -
Late Quaternary geological development of the Jutland Bank and the initiation of the Jutland Current, NE North Sea
(NGU Bulletin (430), Journal article, 1996)Using shallow seismic and core data, a reconstruction has been made of the Late Pleistocene-Early Holocene palaeogeography of Jutland Bank, NE North Sea. A division of Late Pleistocene and Holocene deposits into five ... -
Late-Caledonian structures, differential retrogression and structural position of (ultra)high-pressure rocks in the Nordfjord-Stadlandet area, Western Gneiss Region
(NGU Bulletin (432), Journal article, 1997)Late-Caledonian, amphibolite-facies structures in the Nordfjord-Stadlandet area comprise an 8 km-wide zone of non-coaxial shear below the Nordfjord-Sogn Detachment (NSD). Below this zone, coaxial structures dominate. The ... -
Latest Precambrian and Eocambrian stratigraphy of Norway.
(NGU (251), Journal article, 1967) -
Lead isotope determinations by inductively-coupled plasma mass spectrometry (ICP-MS): potential of sector field instruments
(NGU Bulletin (436), Journal article, 2000)Lead isotope measurements have been carried out using a high-resolution inductively-coupled plasma mass spectrometry (Finnigan MAT ELEMENT, configurated with CD-1 option) The method can be applied to all types of geological ... -
Lead-zinc hydrothermal mineralization in the Pechenga Area, Kola Peninsula, Russia
(NGU Bulletin (423), Journal article, 1992)The Early Proterozoic Pechenga supracrustal belt in the western part of the Kola Peninsula, Russia contains hydrothermal Pb-Zn mineralizations, occurring as veins or sulphide disseminations along hydrothermally altered ... -
Leirfall på Nedremule, Byneset 1943.
(NGU (167), Journal article, 1946)At Nedre Mule in Byneset about 20 km west of Trondheim, a clay slide occurred on the 24th of May 1943, wasting 20 000 sq. m. of cultivated land. The ground slid into the fjord Gulosen. A mud flow was visible in the course ... -
Leirfall ved Aaserumvatnet i Hedrum 1940.
(NGU (167), Journal article, 1946)On the first of July 1940 a clay-slide took place on the beach of lake Aaserumvatnet, 10 km West of Sandefjord. The slide occurred in several repetitions. Commencing at 7 o'clock in the morning the ground was not at rest ... -
Leirfall ved Holund i Grong 1942.
(NGU (167), Journal article, 1946)On january 19th, 1942 a violent clay-slide took place near the farm Holund in Grong district, east of Namsos. The size of the displaced area was about 1 acre. A heavy wave of liquid clay rushed down into a small valley. ... -
Leirfall ved Kulstadsjøen, Vefsnfjorden 1940.
(NGU (167), Journal article, 1946)During the building of the railway line between Mosjøen and Mo in Nordland, the nearly completed work on the ballast was destroyed by a submarine slide on August 31th, 1940. The railway line 3 km north of Mosjøen along the ... -
Leirfall ved Leirnesset, Foldereid 1939-40.
(NGU (167), Journal article, 1946)In the autumn of 1930 a clay-slide took place near Foldereid, Northern Norway. Part of the cross country road to Nordland was touched by the slide. In order to reconstruct the road traverse, borings and ground studies were ... -
Leirfallet ved Knivsvik i Hurum 1940.
(NGU (167), Journal article, 1946)In the night preceding to October 11th, 1940, a clay-slide took place by Knivsvik near Drammen. This was a typical clay-slide; some liquid clay (\"Kvikkleire\") flowed down a brooklet called Knivsvikbekken. Most of the ... -
Leirfallet ved Kverne i Stokke 1944.
(NGU (167), Journal article, 1946)In a marine clay deposit at Kverne in Stokke, near the town of Tønsberg, a great fall of the ground took place on Oct. 9th, 1944. The area hit by the slide amounts to 76 500 sq. metres of well cultivated field. Through a ... -
Leirfallet ved Lade, Trondheim 1944. Foredrag holdt i Norsk Geologisk Forening 11.4.1945
(NGU (167), Journal article, 1946)On April 11. 1944 a clay-slide took place near Ladehammeren N of Trondheim. About 5 acres of the field between Lade Alle and the Ladebekken streamlet slid down. Liquid clay was not visible. There was great uncertainty about ...