Blar i NGU Open Archive på emneord "OMDANNET BERGART"
Viser treff 41-60 av 172
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Fra høifjeldsstrøget mellem Haukeli og Hemsedalsfjeldene
(NGU (36), Journal article, 1903)Foredrag: This mountainous region is situated between latitudes 59\u00B0 50' and 61\u00B0 N in the highest parts of the country. In 1900 Reusch, Bjørlykke and the writer surveyed the western and southern parts of this ... -
Gabbrokonglomeratet i Sjodalen.
(NGU (195), Journal article, 1956)The Gabbor Conglomerate in Sjodalen. The area dealt with in the present paper is a part of the valley of the river Sjoa (Sjodalen) in central southern Norway, about 61o42'N and 9o18'E. An account of the general geology of ... -
Geologi og petrografi på Nord-Karmøy.
(NGU (247), Journal article, 1967)The athor gives a description of rocks and tectonics on the northern and central part of the island of KarmThe athor gives a description of rocks and tectonics on the northern and central part of the island of Karmøy, ... -
Geological and petrographical investigations in the Kongsberg-Bamble formation.
(NGU (160), Journal article, 1943)The rocks of the Kongsberg-Bamble Formation are Pre-Cambrian and belong to the deeper parts of an ancient mountain range (the Sveco-Fennides). The main geological features appear from Table 11. In comparison with the ... -
Geological investigations in the Snåsa-Lurudal area, Nord-Trøndelag.
(NGU (247), Journal article, 1967)Metasediments and meta-volcanic rocks of supposed Middle Ordovician age overlying a basement complex consisting predominantly of granite-gneisses, are described from an area near the north-eastern end of the lake Snåsavatn. ... -
Geological reconnaissance of the area between Kristiansand and Lillesand.
(NGU (205), Journal article, 1959)Randesund-området, et felt på ca. 400 km\u00B2, ligger mellom Lillesand og Kristiansand, dels i Aust-Agder, dels i Vest-Agder fylke. Innen området er det utført petrografisk-tektoniske undersøkelser for Norges Geologiske ... -
Geological studies in the region of Vegarshei - Gjerstad.
(NGU (215), Journal article, 1962) -
Geological studies of the Caledonian pyritic zinc-lead orebody at Bleikvassli, Nordland, Norway.
(NGU (222), Journal article, 1963)Avhandlingen er delt opp i tre deler. Den første del (part 1) gir en detaljert beskrivelse av Bleikvassli malmens mineralogi og petrografi, og malmens geologiske historie forsøkes tolket ved hjelp av dens mineralstrukturer ... -
Geologiske og petrografiske undersøkelser i området Tynset-Femunden.
(NGU (158), Journal article, 1943)The present paper is a description of the geology and petrology of the map quadrangle 38 C, Tynset, in southern Norway. Within the map Tynset we find the border between the large S.E.-Norwegian sparagmite area and the ... -
Geologiske undersøkelser i den sydøstligste del av Helgeland.
(NGU (184), Journal article, 1953)Helgeland is the southern part of northern Norway. The writerand his assistants have worked in the northern part of the area shownon the map, the southern part of the same map is based upon thegeological maps in manuscript ... -
Geologiske Undersøkelser i Espedalen. Gradteig Vinstra og tilgrensende høifjell.
(NGU (163), Journal article, 1945)This paper deals with a group of mountains situated in Espedalen between Vestre Gauldal and Skabu on the map quadrangle F 30 V, Vinstra. The field work was conducted by the author during the summers 1941-42, and -43. This ... -
Geologiske undersøkelser ved Kragerø, Holleia og Troms
(NGU (157), Journal article, 1942) -
Geology and structure of the Prestberget area.
(NGU (228), Journal article, 1964)Prestberget er det berg vest for Vågå kirke (med Jutulporten), hvor veien til Nordherad slynger seg oppover. Ved veien ved Bygdetunet er det meget gode blotninger av lagdelte bergarter og det kan her påvises at lagene er ... -
Granite studies II. The Precambrian Flå granite, a geological and geophysical investigation.
(NGU (219), Journal article, 1963)The Flå granite is composed of two adjacent elliptical granite bodies, the larger northern Hedal granite and the Ådal granite. The granites are surrounded by banded granodioritic gneisses. Migmatites and augen gneisses are ... -
Graptolitførende skifere i vestre Gausdal.
(NGU (1), Journal article, 1891)Forkortet:The Vestre Gausdal is situated in the central part of Southern Norway, 145 kmnorth of Oslo. It lies on the border-zone between the sparagmite-formation,which is Cambrian, and the overlying Silurian schists, which ... -
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 ... -
Gruber og skjerp i kisdraget Øvre Guldal-Tydal.
(NGU (129), Journal article, 1927)The occurences described in this paper form a connection between th mining districts around Røros to the south and those around Meråker to the north. The occurences lie in mountain regions partly above the forest line. The ... -
Grundfjeldstektoniske studier omkring Moss (SØ-Norge). En foreløbig meddelelse.
(NGU (247), Journal article, 1967) -
Grunnfjellet omkring Tangen, østsiden av Mjøsa.
(NGU (211), Journal article, 1960)Petrographic and structural investigations were made in a Precambrian area east of lake Mjøsa, southern Norway. The rocks, mainly granitic and dioritic, are mostly mylonitised and brecciated. Some of the fault zones are ... -
Grunnfjellsvinduer i Dividalen, Troms.
(NGU (223), Journal article, 1963)Two small windows of Precambrian granites were investigated during a few days the summer 1962. Above the granites there follow autochtonous rocks of the Hyolithes Zone, of Lower Cambrian age. On the autochtonous rocks rests ...