Articles | Volume 10, issue 1
https://doi.org/10.5194/se-10-117-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.Anticlockwise metamorphic pressure–temperature paths and nappe stacking in the Reisa Nappe Complex in the Scandinavian Caledonides, northern Norway: evidence for weakening of lower continental crust before and during continental collision
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- Final revised paper (published on 17 Jan 2019)
- Supplement to the final revised paper
- Preprint (discussion started on 31 Jul 2018)
- Supplement to the preprint
Interactive discussion
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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RC1: 'Revie and comments:', Torgeir B. Andersen, 10 Aug 2018
- AC1: 'Response to referee comment by T.B. Andersen', Carly Faber, 20 Nov 2018
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RC2: 'review faber et al.', Thorsten Nagel, 23 Oct 2018
- AC2: 'Response to referee comment by T. Nagel', Carly Faber, 27 Nov 2018
Peer-review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Carly Faber on behalf of the Authors (06 Dec 2018)
Author's response
Manuscript
ED: Publish subject to minor revisions (review by editor) (13 Dec 2018) by Federico Rossetti
AR by Carly Faber on behalf of the Authors (16 Dec 2018)
Author's response
Manuscript
ED: Publish as is (17 Dec 2018) by Federico Rossetti
ED: Publish as is (17 Dec 2018) by Federico Rossetti (Executive editor)
AR by Carly Faber on behalf of the Authors (21 Dec 2018)