Articles | Volume 9, issue 3
https://doi.org/10.5194/se-9-629-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.Pseudotachylyte as field evidence for lower-crustal earthquakes during the intracontinental Petermann Orogeny (Musgrave Block, Central Australia)
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- Final revised paper (published on 09 May 2018)
- Preprint (discussion started on 08 Nov 2017)
Interactive discussion
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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- Supplement
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RC1: 'Review comments', Torgeir B. Andersen, 21 Nov 2017
- AC1: 'Authors response', Friedrich Hawemann, 22 Feb 2018
- SC1: 'Comment self-localizing thermal runaway', Neil Mancktelow, 07 Dec 2017
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RC2: 'Review', Uwe Altenberger, 09 Dec 2017
- AC2: 'Authors response', Friedrich Hawemann, 22 Feb 2018
Peer-review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Friedrich Hawemann on behalf of the Authors (21 Mar 2018)
Author's response
Manuscript
ED: Referee Nomination & Report Request started (22 Mar 2018) by Federico Rossetti
RR by Torgeir B. Andersen (23 Mar 2018)
RR by Uwe Altenberger (28 Mar 2018)
ED: Publish subject to technical corrections (03 Apr 2018) by Federico Rossetti
ED: Publish subject to technical corrections (03 Apr 2018) by Federico Rossetti (Executive editor)
AR by Friedrich Hawemann on behalf of the Authors (05 Apr 2018)
Manuscript