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: 3,659 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,255 1,229 175 3,659 349 149 175
  • HTML: 2,255
  • PDF: 1,229
  • XML: 175
  • Total: 3,659
  • Supplement: 349
  • BibTeX: 149
  • EndNote: 175
Views and downloads (calculated since 07 Nov 2017)
Cumulative views and downloads (calculated since 07 Nov 2017)

Viewed (geographical distribution)

Total article views: 3,659 (including HTML, PDF, and XML) Thereof 3,345 with geography defined and 314 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 21 Nov 2024
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.