Articles | Volume 12, issue 3
https://doi.org/10.5194/se-12-613-2021
https://doi.org/10.5194/se-12-613-2021
Research article
 | 
10 Mar 2021
Research article |  | 10 Mar 2021

The role of edge-driven convection in the generation of volcanism – Part 1: A 2D systematic study

Antonio Manjón-Cabeza Córdoba and Maxim D. Ballmer

Viewed

Total article views: 4,615 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,449 1,036 130 4,615 143 175
  • HTML: 3,449
  • PDF: 1,036
  • XML: 130
  • Total: 4,615
  • BibTeX: 143
  • EndNote: 175
Views and downloads (calculated since 27 Jul 2020)
Cumulative views and downloads (calculated since 27 Jul 2020)

Viewed (geographical distribution)

Total article views: 4,615 (including HTML, PDF, and XML) Thereof 4,401 with geography defined and 214 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 19 Aug 2026
Short summary
The study of intraplate volcanism can inform us about underlying mantle dynamic processes and thermal and/or compositional anomalies. Here, we investigated numerical models of mantle flow and melting of edge-driven convection (EDC), a potential origin for intraplate volcanism. Our most important conclusion is that EDC can only produce moderate amounts of mantle melting. By itself, EDC is insufficient to support the formation of voluminous island-building volcanism over several millions of years.
Share