Middle to Late Devonian–Carboniferous collapse basins on the Finnmark Platform and in the southwesternmost Nordkapp basin, SW Barents Sea

The SW Barents Sea margin experienced a pulse of extensional deformation in the Middle–Late Devonian through the Carboniferous, after the Caledonian Orogeny terminated. These events marked the initial stages of formation of major offshore basins such as the Hammerfest and Nordkapp basins. We mapped...

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Bibliographic Details
Published in:Solid Earth
Main Authors: Koehl, Jean-Baptiste, Bergh, Steffen G, Henningsen, Tormod, Faleide, Jan Inge
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/10852/64811
http://urn.nb.no/URN:NBN:no-67347