Articles | Volume 8, issue 1
https://doi.org/10.5194/se-8-235-2017
https://doi.org/10.5194/se-8-235-2017
Research article
 | 
23 Feb 2017
Research article |  | 23 Feb 2017

The deep Earth origin of the Iceland plume and its effects on regional surface uplift and subsidence

Nicholas Barnett-Moore, Rakib Hassan, Nicolas Flament, and Dietmar Müller

Viewed

Total article views: 3,623 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,797 1,656 170 3,623 171 164 184
  • HTML: 1,797
  • PDF: 1,656
  • XML: 170
  • Total: 3,623
  • Supplement: 171
  • BibTeX: 164
  • EndNote: 184
Views and downloads (calculated since 26 Aug 2016)
Cumulative views and downloads (calculated since 26 Aug 2016)

Viewed (geographical distribution)

Total article views: 3,623 (including HTML, PDF, and XML) Thereof 3,262 with geography defined and 361 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 07 May 2024
Download
Short summary
We use 3D mantle flow models to investigate the evolution of the Iceland plume in the North Atlantic. Results show that over the last ~ 100 Myr a remarkably stable pattern of flow in the lowermost mantle beneath the region resulted in the formation of a plume nucleation site. At the surface, a model plume compared to published observables indicates that its large plume head, ~ 2500 km in diameter, arriving beneath eastern Greenland in the Palaeocene, can account for the volcanic record and uplift.