Articles | Volume 16, issue 10
https://doi.org/10.5194/se-16-1059-2025
https://doi.org/10.5194/se-16-1059-2025
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

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-1826', David Schlaphorst, 25 Jun 2025
  • RC2: 'Comment on egusphere-2025-1826', Pavla Hrubcová, 29 Jul 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Guilherme W. S. de Melo on behalf of the Authors (12 Aug 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (12 Aug 2025) by Simone Pilia
RR by Pavla Hrubcová (13 Aug 2025)
ED: Publish subject to technical corrections (13 Aug 2025) by Simone Pilia
ED: Publish as is (28 Aug 2025) by CharLotte Krawczyk (Executive editor)
AR by Guilherme W. S. de Melo on behalf of the Authors (29 Aug 2025)  Manuscript 
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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.
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