Articles | Volume 12, issue 6
Solid Earth, 12, 1335–1355, 2021
https://doi.org/10.5194/se-12-1335-2021
Solid Earth, 12, 1335–1355, 2021
https://doi.org/10.5194/se-12-1335-2021

Research article 15 Jun 2021

Research article | 15 Jun 2021

Insights from elastic thermobarometry into exhumation of high-pressure metamorphic rocks from Syros, Greece

Miguel Cisneros et al.

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Miguel Cisneros on behalf of the Authors (17 Dec 2020)  Author's response
ED: Referee Nomination & Report Request started (04 Jan 2021) by Federico Rossetti
RR by Valentin Laurent (20 Mar 2021)
ED: Reconsider after major revisions (20 Mar 2021) by Federico Rossetti
AR by Miguel Cisneros on behalf of the Authors (22 Apr 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (review by editor) (29 Apr 2021) by Federico Rossetti
AR by Miguel Cisneros on behalf of the Authors (03 May 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (04 May 2021) by Federico Rossetti
ED: Publish as is (04 May 2021) by Federico Rossetti(Executive Editor)
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Short summary
Constraining the conditions at which rocks form is crucial for understanding geologic processes. For years, the conditions under which rocks from Syros, Greece, formed have remained enigmatic; yet these rocks are fundamental for understanding processes occurring at the interface between colliding tectonic plates (subduction zones). Here, we constrain conditions under which these rocks formed and show they were transported to the surface adjacent to the down-going (subducting) tectonic plate.