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Devonian subduction and syncollisional exhumation of continental crust in Lofoten, Norway
Univ Bonn, Steinmann Inst, D-53115 Bonn, Germany..
Univ Bonn, Steinmann Inst, D-53115 Bonn, Germany..
Slovak Acad Sci, Earth Sci Inst, Dubravska 9, Bratislava 84005 45, Slovakia..
Norwegian Min Museum, Hyttegata 3, N-3602 Kongsberg, Norway..
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2016 (English)In: Geology, ISSN 0091-7613, E-ISSN 1943-2682, Vol. 44, no 3, 223-226 p.Article in journal (Refereed) PublishedText
Abstract [en]

When continents collide, continental crust of the lower plate may be subducted to mantle depth and return to the surface to form eclogite facies metamorphic terranes, as typified by the Western Gneiss Complex of the Scandinavian Caledonides. Proterozoic basement of the Lofoten Islands, located northeast and along strike of the Western Gneiss Complex, contains Caledonian eclogite, although Caledonian deformation is only minor. Previous dating suggested that Lofoten eclogites formed at ca. 480 Ma, i.e., similar to 50 Ma before the collision between the major continents Baltica and Laurentia, and that the Lofoten basement may not originate from Baltica but rather represents a stranded microcontinent. Newly discovered kyanite eclogites from the Lofoten Islands record deep subduction of continental crust during the main (Scandian) stage of Baltica-Laurentia collision ca. 400 Ma. Thermobarometry and thermodynamic modeling yield metamorphic conditions of 2.5-2.8 GPa and similar to 650 degrees C. Lu-Hf geochronology yields 399 +/- 10 Ma, corresponding to the time of garnet growth during subduction. Our results demonstrate that the Lofoten basement belonged to Baltica, was subducted to similar to 90 km depth during the collision with Laurentia, and was exhumed at an intermediate to high rate (>6 mm/yr) while thrusting of a Caledonian allochthon (Leknes Group) was still ongoing. This supports the challenging conclusions that (1) subducted continental crust may stay rigid down to a depth of similar to 90 km, and (2) it may be exhumed during ongoing collision and crustal shortening.

Place, publisher, year, edition, pages
2016. Vol. 44, no 3, 223-226 p.
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URN: urn:nbn:se:uu:diva-282294DOI: 10.1130/G37545.1ISI: 000370934000015OAI: oai:DiVA.org:uu-282294DiVA: diva2:916897
German Research Foundation (DFG), FR700/17-1The Royal Swedish Academy of Sciences
Available from: 2016-04-05 Created: 2016-04-05 Last updated: 2016-04-05Bibliographically approved

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Majka, Jaroslaw
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