Blar i NGU-publikasjoner på tittel
Viser treff 6313-6332 av 7138
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The nature of the basement contact.
(NGU (227), Journal article, 1964)The gneisses below the Cambrian schist or Eocambrian flagstones in the central Norwegian Caledonides have been considered of Precambrian age, but the fact that the contact is always concordant has been explained as due to ... -
The Nickeliferous Iveland-Evje amphibolite and its relation.
(NGU (168a), Journal article, 1947)The pre-Cambrian nickelferous meta-norite at Iveland-Evje represents an amphibolite body entirely surrounded by gneissous granite and augen genisses. More than 90% of the amphibolite body is made up with schistose or ... -
The northern Kongsberg series and its western margin.
(NGU (370), Journal article, 1981)In the Kongsberg Series a major fold interference pattern was established during the Svecofennian orogeny before westward thrusting over the Telemark block developed a margin of ultramylonite (preserved from Flesberg to ... -
The Norwegian groundwater monitoring network (LGN): alkalinity trends in selected aquifers from southern Norway during 1980-1990
(NGU Bulletin (427), Journal article, 1995) -
The Norwegian mining and quarring industry in 2001
(NGU-Rapport (2002.035), Report, 2002)The Norwegian mining and quarring industry had a turnover of approximately NOK 7 billion in 2001 and employed some 5200 workers. It is a major industry in some regions, and the most important counties are Nordland, Møre & ... -
The Norwegian mining and quarrying industry in 2000
(NGU-Rapport (2001.066), Report, 2001)The Norwegian mining and quarrying industry had a turnover of approximately NOK 7 billion in 2000 and employed some 5400 workers. It is a major industry in some regions, and the most important counties are Nordland, Møre ... -
The Ordovician Grøndalsfjell Intrusive Complex: Central Scandinavian Caledonides: field relations, petrography and emplacement
(NGU Bulletin (435), Journal article, 1999)The Grøndalsfjell Intrusive Complex (GIC) is part of a major plutonic province located in the Gjersvik Nappe of the Upper Allochthon in the Caledonides of Central Norway. Field relationships and petrography suggest that ... -
The origin of macrorhytmic units in the Lower Zone of the Lille Kufjord Intrusion, northern Norway.
(NGU Bulletin (420), Journal article, 1990)The Lille Kufjord intrusion is one of the youngest mafic plutons in the Seiland Magmatic Province which forms part of the Middle Allochthon of the North Norwegian Caledonides. It was emplaced at a mid-crustal level into ... -
The Oslo paleorift - A review and guide to excursions. Excursion 2. Nittedal cauldron (Alnsjøen area).
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Excursion 3. Central part of the Oslofjord.
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Excursion 4. Metallogeny associated with the Oslo rifting.
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Excursion 5. Krokskogen lava area.
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Excursion 6. Southern part of the Oslo Rift.
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Geophysical investigations.
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Isotop- and trace-element chemistry, geochronology.
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Metallogeny.
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Petrology of the plutonic rocks.
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Sedimentary rocks associated with the Oslo region lavas.
(NGU (337), Journal article, 1978) -
The Oslo paleorift - A review and guide to excursions. Tectonomagnetic evolution.
(NGU (337), Journal article, 1978)