Subduction and loss of continental crust during the Mesoproterozoic Sveconorwegian Orogeny
Author:
Funder
Norges Forskningsråd
Geological Survey of Norway
Publisher
Elsevier BV
Reference94 articles.
1. Long-term convergence along SW Fennoscandia: 330 m.y. of Proterozoic crustal growth;Åhäll;Precambr. Res.,2008
2. Episodic rapakivi magmatism due to distal orogenesis?: Correlation of 1.69–1.50 Ga orogenic and inboard, “anorogenic” events in the Baltic Shield;Åhäll;Geology,2000
3. Crustal evolution in the SW part of the Baltic Shield: The Hf isotope evidence;Andersen;J. Petrol.,2002
4. Mid-Proterozoic magmatic arc evolution at the southwest margin of the Baltic Shield;Andersen;Lithos,2004
5. Sveconorwegian crustal underplating in southwestern Fennoscandia: LAM-ICPMS U-Pb and Lu-Hf isotope evidence from granites and gneisses in Telemark, southern Norway;Andersen;Lithos,2007
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