Nature of Palaeozoic extension in Lofoten, north Norwegian Continental Shelf: insights from 3-D seismic analysis of a Cordilleran-style metamorphic core complex

Author:

Henstra Gijs Allard1,Rotevatn Atle1

Affiliation:

1. Department of Earth Science; University of Bergen; Allégaten 41 Bergen 5007 Norway

Publisher

Wiley

Subject

Geology

Reference26 articles.

1. Subduction and eduction of continental crust: Major mechanisms during continent-continent collision and orogenic extensional collapse, a model based on the southern Norwegian Caledonides;Andersen;Terra Nova,1991

2. Miocene core complex development and coeval supradetachment basin evolution of Paros, Greece, insights from (U-Th)/He thermochronometry;Bargnesi;Tectonophysics,2013

3. The Lofoten-Vesterålen continental margin: a multiphase Mesozoic-Palaeogene rifted shelf as shown by offshore-onshore brittle fault-fracture analysis;Bergh;Norw. J. Geol.,2007

4. Progressive exhumation during orogenic collapse as indicated by 40Ar/39Ar cooling ages from different structural levels, south-west Norway (abstract);Berry;Geonytt,1995

5. Structural elements of the Norwegian continental shelf. Part II: The Norwegian Sea Region;Blystad;Norw. Petrol. Direct. Bull.,1995

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