Browsing Artikler by Title
Now showing items 808-827 of 1064
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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) -
Strontium isotope composition of the Bindal Batholith, Central Norwegian Caledonides
(NGU Bulletin (423), Journal article, 1992)Forkortet: A strontium isotope study of the Bindal Batholith has been carried out. The data generally do not permit precise and accurate age calculations; however, good estimates for initial Sr ratios are commonly obtained. ... -
Structural evolution of the Bergsdalen Nappes, Southwest Norway
(NGU Bulletin (424), Journal article, 1993)The Bergsdalen nappes are Caledonian thrust sheets which experienced perva- sive, although heterogeneous ductile deformation during the upper green- schist to lowermost amphibolite-facies, Caledonian, thrusting history. ... -
Structural history of the Bygdin area, Oppland.
(NGU (247), Journal article, 1967)The tectonic history of the area, which is part of the marginal thrust zone of the Norwegian Caledonides, is described. Within the area, the Upper Jotun Nappe has been thrust over the Valdres Sparagmite and the Bygdin ... -
Structural interpretation of a double-folded gneiss-amphibolite sequence, Bunnefjorden, Akershus.
(NGU (300), Journal article, 1973)Garnet amphibolite bands folded together with gneiss lamellae in tight to isoclina folds are described. A structural analysis shows that the folds were formed during two separate deformation episodes. This conclusion has ... -
Structural observations from the Kopperå-Riksgrense area and discussi- on of the tectonics of Stjørdalen and the N.E. Trondheim region.
(NGU (245), Journal article, 1967)Minor tectonic structures occurring in weakly metamorphosed Hovin and Horg Group sediments along Tevedalen, east of Meråker, are described in the first part of the paper. Three episodes of folding are recognized, the ... -
Structural setting of two Mesozoic half-grabens off the coast of Trøndelag, Mid-Norwegian shelf
(NGU Bulletin (427), Journal article, 1995) -
Structural succession in a part of the outer Hardangerfjord area, West Norway.
(NGU (343), Journal article, 1978)Recent mapping has made possible a reinterpretation of the tectonostratigraphy of this area, situated at the eastern edge of the \"Faltungsgraben\". It is shown that certain rock units occuring over large areas, and formerly ...