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Basement control of the Caledonian orogen along the Tornetrask section, northern Sweden
Luleå tekniska universitet.
1994 (English)In: Schweizerische Mineralogische und Petrographische Mitteilungen, ISSN 0036-7699, Vol. 74, no 3, p. 469-481Article in journal (Refereed) Published
Abstract [en]

The Scandinavian Caledonides are dominated by orogen-parallel and orogen-transverse structures that have the same strike as old fault zones in the basement of the orogenic foreland. The close correspondence of the rhombohedral fault pattern in the Proterozoic basement with lithologic, structural, and metamorphic discontinuities in the Caledonian nappes suggests that reactivated fault zones in the basement played a major role in the structural evolution of the Scandinavian Caledonides. The orogen-parallel trend is defined by two discontinuous chains of large basement culminations, which are terminated to the north and south against orogen-transverse fault zones

Place, publisher, year, edition, pages
1994. Vol. 74, no 3, p. 469-481
National Category
Geochemistry
Research subject
Applied Geology
Identifiers
URN: urn:nbn:se:ltu:diva-7305Local ID: 5a6fc680-0997-11de-9f31-000ea68e967bOAI: oai:DiVA.org:ltu-7305DiVA, id: diva2:980194
Note

Godkänd; 1994; 20090305 (andbra)

Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2018-02-06Bibliographically approved

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