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Autor:
Kjetil Indrevær, Halldis Lea, Per Terje Osmundsen, Jean-Baptiste P. Koehl, Espen Bergø, Steffen G. Bergh, T.F. Redfield
In the SW Barents Sea, Devonian–Carboniferous collapse led to the formation of major basins and faults, e.g., the Hammerfest Basin bounded by the Troms–Finnmark Fault Complex, and rhomboid- to sigma-shaped (half-)grabens on the Finnmark Platform.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fde2f9af99b26ffe66e8f1d258918001
http://hdl.handle.net/10852/74482
http://hdl.handle.net/10852/74482