Post-entrapment modification of residual inclusion pressure and its implications for Raman elastic thermobarometry

Zhong, Xin; Moulas, Evangelos; Tajčmanová, Lucie

doi:https://doi.org/10.5194/se-11-223-2020

Articles | Volume 11, issue 1

https://doi.org/10.5194/se-11-223-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/se-11-223-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 11, issue 1

Research article

|

25 Feb 2020

Research article |

| 25 Feb 2020

Post-entrapment modification of residual inclusion pressure and its implications for Raman elastic thermobarometry

Xin Zhong, Evangelos Moulas, and Lucie Tajčmanová

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Final revised paper (published on 25 Feb 2020)
Supplement to the final revised paper
Preprint (discussion started on 20 Aug 2019)
Supplement to the preprint

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review on the manuscript “The relaxation of residual inclusion pressure and implications to Raman-thermobarometry” by Zhong et al.', Viktoriya Yarushina, 24 Sep 2019
- AC1: 'Reply to interactive comments by V. Yarushina', Xin Zhong, 25 Nov 2019
RC2: 'Review of Zhong et al', Anonymous Referee #2, 05 Nov 2019
- AC2: 'Reply to interactive comments by referee #2', Xin Zhong, 25 Nov 2019

Peer-review completion

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

AR by Xin Zhong on behalf of the Authors (25 Nov 2019) Author's response Manuscript

ED: Referee Nomination & Report Request started (20 Dec 2019) by Taras Gerya

RR by Viktoriya Yarushina (06 Jan 2020)

RR by Anonymous Referee #2 (20 Jan 2020)

ED: Publish as is (20 Jan 2020) by Taras Gerya

ED: Publish as is (20 Jan 2020) by Susanne Buiter (Executive editor)

AR by Xin Zhong on behalf of the Authors (25 Jan 2020) Manuscript

Short summary

In this study, we present a 1-D visco-elasto-plastic model in a spherical coordinate system to study the residual pressure preserved in mineral inclusions. This allows one to study how much residual pressure can be preserved after viscous relaxation. An example of quartz inclusion in garnet host is studied and it is found that above 600–700 °C, substantial viscous relaxation will occur. If one uses the relaxed residual quartz pressure for barometry, erroneous results will be obtained.