Solid Earth
Solid Earth
SE
Articles | Volume 16, issue 10
Articles | Volume 16, issue 10
https://doi.org/10.5194/se-16-1059-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-16-1059-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 10
Research article
 | 
10 Oct 2025
Research article |  | 10 Oct 2025

Seismicity and thermal structure of the St. Paul Transform System, equatorial Atlantic: insights from focal depth analysis

Guilherme W. S. de Melo, Ingo Grevemeyer, Sibiao Liu, Marcia Maia, and Lars Rüpke

Viewed

Total article views: 4,633 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,533 917 183 4,633 160 147 180
  • HTML: 3,533
  • PDF: 917
  • XML: 183
  • Total: 4,633
  • Supplement: 160
  • BibTeX: 147
  • EndNote: 180
Views and downloads (calculated since 13 May 2025)
Cumulative views and downloads (calculated since 13 May 2025)

Viewed (geographical distribution)

Total article views: 4,633 (including HTML, PDF, and XML) Thereof 4,542 with geography defined and 91 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Saved (final revised paper)

Latest update: 12 Aug 2026
Download
Short summary
The St. Paul Transform System on the equatorial Atlantic is a seismically oceanic transform fault system. This study re-examines the focal depths of 35 earthquakes (MW 5.3–6.9) from Transforms A, B, and C. The data suggest that the seismogenic zone ranges from 5 to 18 km deep, with the deepest occurring in cooler lithosphere around the center of the transform segments. This challenges earlier hypotheses and indicates a global pattern of cooler mantle in center of oceanic transform faults.
Read more
Share