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SE | Articles | Volume 11, issue 2
Solid Earth, 11, 307–328, 2020
https://doi.org/10.5194/se-11-307-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Exploring new frontiers in fluids processes in subduction...

Solid Earth, 11, 307–328, 2020
https://doi.org/10.5194/se-11-307-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 10 Mar 2020

Research article | 10 Mar 2020

Tracing fluid transfers in subduction zones: an integrated thermodynamic and δ18O fractionation modelling approach

Alice Vho et al.

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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 Anna Mirena Feist-Polner on behalf of the Authors (16 Jan 2020)  Author's response
ED: Publish as is (17 Jan 2020) by Nadia Malaspina
ED: Publish as is (18 Jan 2020) by Federico Rossetti(Executive Editor)
AR by Alice Vho on behalf of the Authors (20 Jan 2020)  Author's response

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Alice Vho on behalf of the Authors (12 Feb 2020)   Author's adjustment   Manuscript
EA: Adjustments approved (05 Mar 2020) by Nadia Malaspina
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Short summary
This study presents an approach that combines equilibrium thermodynamic modelling with oxygen isotope fractionation modelling for investigating fluid–rock interaction in metamorphic systems. An application to subduction zones shows that chemical and isotopic zoning in minerals can be used to determine feasible fluid sources and the conditions of interaction. Slab-derived fluids can cause oxygen isotope variations in the mantle wedge that may result in anomalous isotopic signatures of arc lavas.
This study presents an approach that combines equilibrium thermodynamic modelling with oxygen...
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