Blar i Artikler på tittel
Viser treff 801-820 av 1064
-
Statsgeologenes årsberetninger for 1923. Geologiske optegnelser fra Troldhetta rektangelblad.
(NGU (122), Journal article, 1924) -
Statsgeologenes årsberetninger for 1923. I. Grongdistriktet. II. Vanntunnelen Tunhøvd-Nore. III. Utsjøgruben ved Eidsvoll gullverk.
(NGU (122), Journal article, 1924) -
Statsgeologenes årsberetninger for 1923. Skjellbanker i Lørenskog.
(NGU (122), Journal article, 1924) -
Stilbite, stellerite, and laumontite at Honningsvåg, Magerø, norhtern Norway.
(NGU (205), Journal article, 1959)Prøver fra to lokalitetet ved Honningsvåg, Magerø, Nord-Norge, inneholder zeoliter. Desmin og stellerit forekommer i en sleppefylling i Eokambrisk skifer på Juldagsneset, SØ for Honningsvåg, og laumontit i en sleppefylling ... -
Storisens transport av kisblokker fra Joma.
(NGU (203), Journal article, 1958)For three summers the Geological Survey of Norway has carried out a special hunt of pyrite boulders within the Grong area and adjacent districts. One result is the establishement of a marked boulder train from the Joma ... -
Strandfladen, et nyt træk i Norges geografi
(NGU (14), Journal article, 1894)Forkortet: The western slopes of the Scandinavian peninsula do not generally extend quite to the sea; but we see there low almost level parts, which the author calls the Norwegian coast plain. The figures on pp. 1 and 2 ... -
Strandliniens beliggenhed under stenalderen i det sydøstlige Norge
(NGU (41), Journal article, 1905)Forkortet: Die Lage der Strandlinie w\u00E4hrend der verschieden Abschnitte der postglacialen Hebung. Zur L\u00F6sung dieser Aufgabe wurde eine Revision der fr\u00FCheren Untersuch- ungen \u00FCber die gleichzeitigen ... -
Strandlinjer og isavsmelting i midtre Hardanger, Vest-Norge.
(NGU (387), Journal article, 1983)In the Hardangerfjord area a shore-line diagram has been constructed on the basis of an earlier established shore-displacement diagram from Bømlo and 14C-dated marine levels from Stamnes, Bu and Eidfjord. Data from ... -
Strandlinjer, moræner og skjælforekomster i den sydlige del av Troms fylke
(NGU (94), Journal article, 1922)Within the Ofoten territory there are 5 good shore-lines as elsewhere in Northern Norway and besides these there is a 6th line farther to the north only observed near the heads of the fjords. These 6 lines have been measured ... -
Strategies for groundwater prospecting in hard rocks: a probabilistic approach
(NGU Bulletin (439), Journal article, 2002)Private wells in fractured, Precambrian, crystlline rocks are important for rural areas and small communities in Sweden. Since well yields normally are small, systematic approaches to groundwater prospecting are required ... -
Stratigraphical consequences of the discovery of Silurian fossils on Magerøy, the island of North Cape.
(NGU (247), Journal article, 1967)Crionid stems were discovered east of Norvågen (east of Honningsvåg) on Magerøy in 1939. In 1960 an additional find of fossils proved a Silurian age for the limestone and conglomerate beds there. Two years later the athor ... -
Stratigraphical position of the Gudå conglomerate zone.
(NGU (227), Journal article, 1964)The Gudå conglomerate zone has been considered to be of Upper Ordovician to Lower Silurian age. The main argument for this conclusion has been that the conglomerates of this zone have been the same pebble composition as ... -
Stratigraphy and major structures of the Grong District, Nord- Trøndelag.
(NGU (354), Journal article, 1979)The rock sequence of the Grong district, which occurs in a depression within the Norwegian Caledonides between two Precambrian massifs, Børgefjell to the north and the Grong culmination in the south, can be divided into ... -
Stratigraphy and structure of eocambrian and younger deposits in a part of the Gudbrandsdal valley district, south Norway.
(NGU (251), Journal article, 1967)A sequence of five separable formations of assumed Eocambrian to Cambrian and earliest Ordovician age are separated by a thrust-plane from the overlying Otta nappe. A lowermost formation of alternating schists and sandstones ... -
Stratigraphy and structure of the northern part of the Repparfjord - Komagfjord window, Finnmark, Northern Norway.
(NGU (377), Journal article, 1983)In the northern district of the Repparfjord-Komagfjord Window, supracrustal and intrusive rocks of Early Proterozoic age are unconformably overlain by a thin sequence of Vendian sediments. Both of these units are overthrust ... -
Stratigraphy and structure of the Ringebu - Vinstra district, Gudbrandsdalen; with a short analysis of the western part of the sparagmite region.
(NGU (293), Journal article, 1973)The Ringebu-Vinstra district, Gudbrandsdalen, is one in which several of the main structural units in Southern Norway come together. Essentially, the rocks belong to three main tectonic units: 1. Parautochthonous rocks of ... -
Stratigraphy of the Otta-Vågå tract and regional stratigraphic implications
(NGU Bulletin (427), Journal article, 1995) -
Stratigraphy of the Sparagmite Group, including "the sandstone divisi- ons of Finnmark".
(NGU (208), Journal article, 1960)