Articles | Volume 16, issue 6
https://doi.org/10.5194/se-16-579-2025
https://doi.org/10.5194/se-16-579-2025
Research article
 | 
30 Jun 2025
Research article |  | 30 Jun 2025

Accretionary prism deformation and fluid migration caused by slow earthquakes in the Nankai subduction zone

Takashi Tonegawa, Takeshi Akuhara, Yusuke Yamashita, Hiroko Sugioka, Masanao Shinohara, Shunsuke Takemura, and Takeshi Tsuji

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2024-3405', Takashi Hirose, 24 Dec 2024
    • AC3: 'Reply on CC1', Takashi Tonegawa, 17 Mar 2025
  • RC1: 'Review Comment on egusphere-2024-3405', Takashi Hirose, 24 Dec 2024
    • AC1: 'Reply on RC1', Takashi Tonegawa, 17 Mar 2025
  • RC2: 'Comment on egusphere-2024-3405', Manuela Köpfli, 13 Jan 2025
    • AC2: 'Reply on RC2', Takashi Tonegawa, 17 Mar 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Takashi Tonegawa on behalf of the Authors (19 Mar 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (27 Mar 2025) by Irene Bianchi
RR by Anonymous Referee #2 (27 Mar 2025)
ED: Publish as is (02 Apr 2025) by Irene Bianchi
ED: Publish as is (02 Apr 2025) by CharLotte Krawczyk (Executive editor)
AR by Takashi Tonegawa on behalf of the Authors (07 Apr 2025)  Author's response   Manuscript 
Download
Short summary
This study demonstrates that for slow earthquakes in the shallow Nankai subduction zone, (1) the seismic velocity reductions in the accretionary prism reflect the stress field changes due to the slow earthquakes, and (2) the temporal variations in the heterogeneous structure correspond to upward fluid migrations from the source region of the slow earthquakes.
Share