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Viser treff 290-309 av 1064
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Geologiske undersøkelser i sørlige Helgeland og nordlige Namdal.
(NGU (254), Journal article, 1967)Cambro-Silurian rocks with large intrusive masses cover most of the area. In the south-westernmost part there are also deeper lying rocks. This part is referred to as the basal gneiss region, while the rest of the area is ... -
Geologiske undersøkelser ved Kragerø, Holleia og Troms
(NGU (157), Journal article, 1942) -
Geology and K/Ar chronology of the Målvika scheelite skarns, Central Norwegian Caledonides.
(NGU Bulletin (424), Journal article, 1993)Skarns present on the northern shore of Tosenfjord overprint the S2 fabric of the adjacent gneiss (which formed during peak regional metamorphism). Together with petrographic evidence of the late crystallization of sheelite, ... -
Geology and metamorphic evolution of the Roan area, Vestranden, Western Gneiss Region, Central Norwegian Caledonides.
(NGU Bulletin (413), Journal article, 1988)Forkortet.In the gneiss area of northern Vestranden, kilometre-scale upright domes andbasins refold tight and isoclinal folds of banded amphibolite facies ortho-gneisses and supracrustal rocks. In the Roan area, a major ... -
Geology and petrochemistry of the Smøla-Hitra Batholith, Central Norway.
(NGU Bulletin (416), Journal article, 1989)The plutonic rocks which compose the Smøla-Hitra Batholith (SHB) cover an exposed area of c.1000 km\u00B2 and intrude folded, Arenig-Llanvirn, low-grade meta-sedimentary and bimodal metavolcanic rocks and higher-grade ... -
Geology and structural evolution of the Precambrian rocks of the Oslofjord - Øyeren area, Southeast Norway.
(NGU Bulletin (398), Journal article, 1984)The area (1200 km\u00B2) described covers the northern part of a major thrust segment in the eastern subprovince of the Sveonorwegian orogenic belt along the southwestern margin of the Baltic Shield. The oldest rock unit ... -
Geology and structure of Gjerby, Nordland.
(NGU (370), Journal article, 1981)The island of Gjerøy is made up of acid gneisses with subordinate mixed gneisses which are tightly interfolded with banded gneisses and associated metasediments. The early tight folds are refolded to produce a large-scale ... -
Geology and structure of the area west of Fyresvatn, Telemark, southern Norway. The Precambrian rocks of the Telemark area in South Central Norway no. X.
(NGU (268), Journal article, 1970)Geological mapping has shown that the area west of Fyresvatn, Telemark, Southern Norway, is underlain by a sequence of gneisses, quartz schists, amphibolites, migmatites and epidote bearing quartzite, together with a ... -
Geology and structure of the Beito Window, Valdres.
(NGU (327), Journal article, 1976)Three groups of Caledonian nappes sit directly on Precambrian gneisses. The lowest nappe consists of generally upward-facing parautochthonous or allochthonous Cambro-Ordovician quartizites and phyllites. The middle nappe ... -
Geology and structure of the Bjøllånes area, Rana, Nordland.
(NGU (343), Journal article, 1978)The field relationships of rock groups of three tectonic units from the area west of the Lønsdalen basal massif are outlined and the lithologies and mineral assemblages are described. Chemical analyses of marbles and ... -
Geology and structure of the Dombås-Lesja area, southern Trondheim region, south-central Norway.
(NGU (340), Journal article, 1978)Investigations in the southernmost part of the Trondheim region have established the presence of a new tectonic unit, the Andbergshøi Complex, interposed between the Trondheim Nappe and the Western Precambrian basement. ... -
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 ... -
Geology of Moskenesøy, Lofoten, North Norway.
(NGU (270), Journal article, 1971)Moskenesøy, Lofoten, forms part of the Lofoten-Vesterålen Precambrian high grade granulite metamorphic province. The dominant basal rock type of the island is a porphyroblastic monzonitic gneiss interbanded with, and grading ... -
Geology of the Altenes area, Alta-Kvænangen window, North Norway.
(NGU (351), Journal article, 1979)Precambrian supracrustal and intrusive rocks of the Raipas Group of supposed Karelian age are unconformably overlain by Vendian to ?Lower Cambrian sedimentary rocks, which have in turn been overridden by allochthonous rocks ... -
Geology of the Båtsfjordfjellet drillcore, Varanger Peninsula, Finnmark, northern Norway
(NGU Bulletin (452), Journal article, 2012)Logging of >800 metres of drillcore from a borehole on Båtsfjordfjellet, Varanger Peninsula, revealed a succession of very low-grade, metasedimentary rocks which are assigned to specific Neoproterozoic formations recognisable ... -
Geology of the eastern part of the Meråker area.
(NGU (245), Journal article, 1967)Within the mapped area slightly metamorphosed clastic sediments occur, probably of Upper Ordovician and Silurian age. The author describes a metagreywacke-slate association with metaconglomerates and gabbrodiorite sills, ... -
Geology of the Folldal area, southern Trondheim Region Caledonides, Norway.
(NGU Bulletin (426), Journal article, 1994)The lowest stratigraphic unit in the Folldal area is the Gula Group, comprising turbidites and minor greenstones in the lower part (the Singsås Formation) and graphitic pelites with subordinate marble and conglomerate in ... -
Geology of the Hølonda-Hulsjøen area, Trondheim region.
(NGU (266), Journal article, 1970)The geology of the area south of Trondheim is described. A new stratigraphical division of the Early Palaeozoic is proposed and its structure outlined. The entire Early Palaeozoic sedimentary and volcanic complex has been ... -
Geology of the Iesjav'ri-Skoganvarre area, Northern Finnmarksvidda, North Norway.
(NGU Bulletin (403), Journal article, 1985)The Iesjav'ri-Skoganvarre areas is located in the northern part ofFinnmarksvidda and its underlain by Archaean-Early Proterozoic rocks. Theoldest unit, the Jer'gul Gneiss Complex, is unconformably overlain bymetasediments ... -
Geology of the Meråker area as a key to the eastern part of the Trondheim region.
(NGU (245), Journal article, 1967)The present paper deals with a discussion of the main tectono-stratigraphical problems of the eastern Trondheim region. Based on detailed studies made in the Meråker area in the last three summers and available manuscript ...