Articles | Volume 9, issue 2
https://doi.org/10.5194/se-9-341-2018
https://doi.org/10.5194/se-9-341-2018
Research article
 | 
28 Mar 2018
Research article |  | 28 Mar 2018

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

Jean-Baptiste P. Koehl, Steffen G. Bergh, Tormod Henningsen, and Jan Inge Faleide

Viewed

Total article views: 4,011 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,465 1,357 189 4,011 384 178 232
  • HTML: 2,465
  • PDF: 1,357
  • XML: 189
  • Total: 4,011
  • Supplement: 384
  • BibTeX: 178
  • EndNote: 232
Views and downloads (calculated since 07 Nov 2017)
Cumulative views and downloads (calculated since 07 Nov 2017)

Viewed (geographical distribution)

Total article views: 4,011 (including HTML, PDF, and XML) Thereof 3,691 with geography defined and 320 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 07 Oct 2025
Download
Short summary
The goal of this work is to study large cracks in the Earth's crust called faults near the coast of northern Norway in the SW Barents Sea. We interpreted seismic data (equivalent to X-ray diagram of the Earth) that showed the presence of a large fault near the coast of Norway, which contributed to building the mountain chain observed in Norway and later helped open the North Atlantic Ocean, separating Greenland from Norway.
Share