Articles | Volume 18, issue 5
https://doi.org/10.5194/essd-18-3177-2026
https://doi.org/10.5194/essd-18-3177-2026
Data description article
 | 
13 May 2026
Data description article |  | 13 May 2026

The new seismic catalog of the Gargano area (Southern Italy) after a decade of seismic monitoring by OTRIONS network

Andrea Pio Ferreri, Annalisa Romeo, Rossella Giannuzzi, Teresa Ninivaggi, Marilena Filippucci, Gianpaolo Cecere, Luigi Falco, Maddalena Michele, Giulio Selvaggi, and Andrea Tallarico

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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 essd-2025-335', Dino Bindi, 14 Sep 2025
    • AC2: 'Reply on RC1', Marilena Filippucci, 05 Dec 2025
  • RC2: 'Comment on essd-2025-335', Anonymous Referee #2, 05 Nov 2025
    • AC1: 'Reply on RC2', Marilena Filippucci, 05 Dec 2025

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Marilena Filippucci on behalf of the Authors (05 Dec 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (17 Dec 2025) by Andrea Rovida
RR by Dino Bindi (01 Jan 2026)
RR by Anonymous Referee #2 (02 Jan 2026)
ED: Publish subject to minor revisions (review by editor) (07 Jan 2026) by Andrea Rovida
AR by Marilena Filippucci on behalf of the Authors (16 Jan 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (05 Feb 2026) by Andrea Rovida
AR by Marilena Filippucci on behalf of the Authors (17 Feb 2026)  Manuscript 

Post-review adjustments

AA – Author's adjustment | EA – Editor approval
AA by Marilena Filippucci on behalf of the Authors (07 May 2026)   Author's adjustment   Manuscript
EA: Adjustments approved (08 May 2026) by Andrea Rovida
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Short summary
The Gargano Promontory (Italy) has been monitored by the University of Bari seismic network since 2013, which has supported civil protection since 2019. Ten years of data were reanalyzed using automatic methods, detecting more than 7100 events. After manual review, 4098 were confirmed as earthquakes. Their locations, deep in the crust, suggest a potentially hazardous structure that requires further investigation.
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