Fault-controlled dolomitization in the Montagna dei Fiori Anticline (Central Apennines, Italy): record of a dominantly pre-orogenic fluid migration

Mozafari, Mahtab; Swennen, Rudy; Balsamo, Fabrizio; El Desouky, Hamdy; Storti, Fabrizio; Taberner, Conxita

doi:https://doi.org/10.5194/se-10-1355-2019

Articles | Volume 10, issue 4

https://doi.org/10.5194/se-10-1355-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/se-10-1355-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 10, issue 4

Research article

| Highlight paper

|

20 Aug 2019

Research article | Highlight paper |

| 20 Aug 2019

Fault-controlled dolomitization in the Montagna dei Fiori Anticline (Central Apennines, Italy): record of a dominantly pre-orogenic fluid migration

Mahtab Mozafari, Rudy Swennen, Fabrizio Balsamo, Hamdy El Desouky, Fabrizio Storti, and Conxita Taberner

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Final revised paper (published on 20 Aug 2019)
Preprint (discussion started on 03 Jan 2019)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review of se-2018-136', Jim Hendry, 23 Jan 2019
- AC1: 'Revision', Mahtab Mozafari, 20 Feb 2019
- AC2: 'Revision', Mahtab Mozafari, 22 Feb 2019
  - RC2: 'Review of se-2018-136', Jim Hendry, 01 Mar 2019
    - AC3: 'Replay', Mahtab Mozafari, 02 Mar 2019
      - RC3: 'Dolomitising fluid volumes', Jim Hendry, 02 Mar 2019
        
        AC5: 'Replay', Mahtab Mozafari, 30 Apr 2019
RC4: 'Estibalitz Ukar_revision', Estibalitz Ukar, 21 Mar 2019
- AC4: 'Revision', Mahtab Mozafari, 25 Apr 2019

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Mahtab Mozafari on behalf of the Authors (26 May 2019)

ED: Publish as is (17 Jul 2019) by Elias Samankassou

ED: Publish as is (17 Jul 2019) by Elias Samankassou (Executive editor)

AR by Mahtab Mozafari on behalf of the Authors (24 Jul 2019) Manuscript

Short summary

The dolomitized intervals of the Lower Jurassic deposits exposed in the Montagna dei Fiori Anticline (Central Apennines, Italy) have been investigated. Accordingly, two fault-related dolomitization events were recognised and interpreted as having occurred before and during the Apenninic orogeny. The analyses suggest significant involvement of evaporitic fluids in both events, most likely derived from the underlying Upper Triassic Burano Formation in the detachment level.