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Ductile rebound of an orogenic root: case study and numerical model of gravity tectonics in the Western Gneiss Complex, Caledonides, southern Norway
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2000 (English)In: TERRA NOVA, ISSN 0954-4879, Vol. 12, no 1, 1-7 p.Article in journal (Refereed) Published
Abstract [en]

The main Caledonian deformation in the Western Gneiss Complex (southern Norway) has been interpreted as resulting from the gravity-driven ductile rebound of the orogenic root. Detailed field data from the Sognefjord profile, a 60-km long, continuously exp

Place, publisher, year, edition, pages
BLACKWELL SCIENCE LTD , 2000. Vol. 12, no 1, 1-7 p.
Keyword [en]
CRUSTAL; SOGNEFJORD; GROWTH; BELTS
Identifiers
URN: urn:nbn:se:uu:diva-37734OAI: oai:DiVA.org:uu-37734DiVA: diva2:65633
Note
Addresses: Milnes AG, GEA Consulting, Box 1301, SE-75143 Uppsala, Sweden. GEA Consulting, SE-75143 Uppsala, Sweden. Uppsala Univ, Dept Earth Sci, Hans Ramberg Tecton Lab, SE-75236 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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