Articles | Volume 13, issue 1
https://doi.org/10.5194/se-13-205-2022
https://doi.org/10.5194/se-13-205-2022
Research article
 | 
27 Jan 2022
Research article |  | 27 Jan 2022

Structural complexities and tectonic barriers controlling recent seismic activity in the Pollino area (Calabria–Lucania, southern Italy) – constraints from stress inversion and 3D fault model building

Daniele Cirillo, Cristina Totaro, Giusy Lavecchia, Barbara Orecchio, Rita de Nardis, Debora Presti, Federica Ferrarini, Simone Bello, and Francesco Brozzetti

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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 se-2021-76', Anonymous Referee #1, 16 Jul 2021
    • AC1: 'Reply on RC1', Daniele Cirillo, 31 Aug 2021
  • RC2: 'Comment on se-2021-76', Barreca Giovanni, 18 Jul 2021
    • AC2: 'Reply on RC2', Daniele Cirillo, 31 Aug 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Daniele Cirillo on behalf of the Authors (13 Nov 2021)  Author's response   Author's tracked changes 
EF by Sarah Buchmann (25 Nov 2021)  Manuscript 
EF by Sarah Buchmann (25 Nov 2021)  Supplement 
ED: Publish subject to minor revisions (review by editor) (28 Nov 2021) by Massimiliano Porreca
AR by Daniele Cirillo on behalf of the Authors (03 Dec 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (07 Dec 2021) by Massimiliano Porreca
ED: Publish subject to technical corrections (07 Dec 2021) by Federico Rossetti (Executive editor)
AR by Daniele Cirillo on behalf of the Authors (10 Dec 2021)  Author's response   Manuscript 
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Short summary
The Pollino region is a highly seismic area of Italy. Increasing the geological knowledge on areas like this contributes to reducing risk and saving lives. We reconstruct the 3D model of the faults which generated the 2010–2014 seismicity integrating geological and seismological data. Appropriate relationships based on the dimensions of the activated faults suggest that they did not fully discharge their seismic potential and could release further significant earthquakes in the near future.