Articles | Volume 13, issue 6
Solid Earth, 13, 957–974, 2022
https://doi.org/10.5194/se-13-957-2022
Solid Earth, 13, 957–974, 2022
https://doi.org/10.5194/se-13-957-2022
Research article
03 Jun 2022
Research article | 03 Jun 2022

Aegean-style extensional deformation in the contractional southern Dinarides: incipient normal fault scarps in Montenegro

Peter Biermanns et al.

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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-2021-97', Gerald P. Roberts, 11 Aug 2021
    • AC3: 'Final response on RC1', Peter Biermanns, 14 Dec 2021
    • AC4: 'Final response on RC1', Peter Biermanns, 14 Dec 2021
  • AC1: 'Comment on se-2021-97', Peter Biermanns, 24 Aug 2021
  • RC2: 'Comment on se-2021-97', Lucilla Benedetti, 11 Oct 2021
    • AC5: 'Final response on RC2', Peter Biermanns, 14 Dec 2021
  • AC2: 'Comment on se-2021-97', Peter Biermanns, 05 Nov 2021
    • RC3: 'Reply on AC2', Gerald P. Roberts, 20 Dec 2021
      • AC6: 'Reply on RC3', Peter Biermanns, 10 Feb 2022
  • RC4: 'Comment on se-2021-97', Anonymous Referee #3, 17 Jan 2022
    • AC7: 'Reply on RC4', Peter Biermanns, 10 Feb 2022
  • EC1: 'Comment on se-2021-97', Federico Rossetti, 13 Feb 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Peter Biermanns on behalf of the Authors (06 Mar 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (07 Mar 2022) by Federico Rossetti
RR by Anonymous Referee #4 (07 Apr 2022)
RR by Luigi Ferranti (11 Apr 2022)
ED: Publish subject to minor revisions (review by editor) (12 Apr 2022) by Federico Rossetti
AR by Peter Biermanns on behalf of the Authors (29 Apr 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (02 May 2022) by Federico Rossetti
ED: Publish as is (02 May 2022) by Federico Rossetti(Executive Editor)
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Short summary
We introduce two up to 7 km long normal fault scarps near the city of Bar (Montenegro). The fact that these widely visible seismogenic structures have never been described before is even less surprising than the circumstance that they apparently do not fit the tectonic setting that they are located in. By quantifying the age and movement of the newly discovered fault scarps and by partly re-interpreting local tectonics, we introduce approaches to explain how this is still compatible.