Articles | Volume 11, issue 2
https://doi.org/10.5194/se-11-307-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-11-307-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Mar 2020
Research article |
| 10 Mar 2020
| 10 Mar 2020
Tracing fluid transfers in subduction zones: an integrated thermodynamic and δ18O fractionation modelling approach
Alice Vho
CORRESPONDING AUTHOR
Institute of Geological Sciences, University of Bern, 3012 Bern,
Switzerland
Pierre Lanari
Institute of Geological Sciences, University of Bern, 3012 Bern,
Switzerland
Daniela Rubatto
Institute of Geological Sciences, University of Bern, 3012 Bern,
Switzerland
Institut de Sciences de la Terre, University of Lausanne, 1015
Lausanne, Switzerland
Jörg Hermann
Institute of Geological Sciences, University of Bern, 3012 Bern,
Switzerland
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Cited
18 citations as recorded by crossref.
- A rutile and titanite record of subduction fluids: Integrated oxygen isotope and trace element analyses in Franciscan high‐pressure rocks F. Page & C. Storey 10.1111/jmg.12717
- Trace element and isotopic zoning of garnetite veins in amphibolitized eclogite, Franciscan Complex, California, USA A. Cruz-Uribe et al. 10.1007/s00410-021-01795-4
- Pervasive fluid-rock interaction in subducted oceanic crust revealed by oxygen isotope zoning in garnet T. Bovay et al. 10.1007/s00410-021-01806-4
- A new insight into metasomatism through mass-density-solid volume variation maps S. Centrella 10.1016/j.chemer.2023.126043
- Some thoughts about eclogites and related rocks M. Brown 10.5194/ejm-35-523-2023
- Olivine formation processes and fluid pathways in subducted serpentinites revealed by in-situ oxygen isotope analysis (Zermatt-Saas, Switzerland) M. Ulrich et al. 10.1016/j.chemgeo.2024.121978
- Decoupled Zircon Si–O Isotopes Tracing the Supracrustal Silicification and Komatiitic‐Derived Fluids in the Source of TTGs K. Lei et al. 10.1029/2023GL104002
- An Internally-Consistent Database for Oxygen Isotope Fractionation Between Minerals A. Vho et al. 10.1093/petrology/egaa001
- Origin of Crystals in Mafic to Intermediate Magmas from Circum-Pacific Continental Arcs: Transcrustal Magmatic Systems Versus Transcrustal Plutonic Systems G. Zellmer et al. 10.1093/petrology/egae013
- Tracing fluid infiltration into oceanic crust up to ultra-high-pressure conditions D. Rubatto et al. 10.1007/s00410-023-02060-6
- OH incorporation and retention in eclogite-facies garnets from the Zermatt–Saas area (Switzerland) and their contribution to the deep water cycle J. Reynes et al. 10.5194/ejm-35-679-2023
- Garnet zoning patterns record multiple processes of chemical transfer during subduction F. George et al. 10.1016/j.epsl.2024.118634
- An introductory review of the thermal structure of subduction zones: I—motivation and selected examples P. van Keken & C. Wilson 10.1186/s40645-023-00573-z
- Channelized CO2-Rich Fluid Activity along a Subduction Interface in the Paleoproterozoic Wutai Complex, North China Craton B. Wang et al. 10.3390/min11070748
- Zircon U-Pb and geochemical signatures in high-pressure, low-temperature metamorphic rocks as recorders of subduction zone processes, Sikinos and Ios islands, Greece E. Poulaki et al. 10.1016/j.chemgeo.2021.120447
- Rheology modification in a subduction channel due to eclogite facies metasomatism (Rocky Beach Metamorphic Mélange, Port Macquarie, Australia) M. Finch et al. 10.1016/j.lithos.2024.107797
- A review of the geochemical changes occurring during metamorphic devolatilization of metasedimentary rocks A. Stepanov 10.1016/j.chemgeo.2021.120080
- Greenstone burial–exhumation cycles at the late Archean transition to plate tectonics Z. Ivan et al. 10.1038/s41467-022-35208-2
17 citations as recorded by crossref.
- A rutile and titanite record of subduction fluids: Integrated oxygen isotope and trace element analyses in Franciscan high‐pressure rocks F. Page & C. Storey 10.1111/jmg.12717
- Trace element and isotopic zoning of garnetite veins in amphibolitized eclogite, Franciscan Complex, California, USA A. Cruz-Uribe et al. 10.1007/s00410-021-01795-4
- Pervasive fluid-rock interaction in subducted oceanic crust revealed by oxygen isotope zoning in garnet T. Bovay et al. 10.1007/s00410-021-01806-4
- A new insight into metasomatism through mass-density-solid volume variation maps S. Centrella 10.1016/j.chemer.2023.126043
- Some thoughts about eclogites and related rocks M. Brown 10.5194/ejm-35-523-2023
- Olivine formation processes and fluid pathways in subducted serpentinites revealed by in-situ oxygen isotope analysis (Zermatt-Saas, Switzerland) M. Ulrich et al. 10.1016/j.chemgeo.2024.121978
- Decoupled Zircon Si–O Isotopes Tracing the Supracrustal Silicification and Komatiitic‐Derived Fluids in the Source of TTGs K. Lei et al. 10.1029/2023GL104002
- An Internally-Consistent Database for Oxygen Isotope Fractionation Between Minerals A. Vho et al. 10.1093/petrology/egaa001
- Origin of Crystals in Mafic to Intermediate Magmas from Circum-Pacific Continental Arcs: Transcrustal Magmatic Systems Versus Transcrustal Plutonic Systems G. Zellmer et al. 10.1093/petrology/egae013
- Tracing fluid infiltration into oceanic crust up to ultra-high-pressure conditions D. Rubatto et al. 10.1007/s00410-023-02060-6
- OH incorporation and retention in eclogite-facies garnets from the Zermatt–Saas area (Switzerland) and their contribution to the deep water cycle J. Reynes et al. 10.5194/ejm-35-679-2023
- Garnet zoning patterns record multiple processes of chemical transfer during subduction F. George et al. 10.1016/j.epsl.2024.118634
- An introductory review of the thermal structure of subduction zones: I—motivation and selected examples P. van Keken & C. Wilson 10.1186/s40645-023-00573-z
- Channelized CO2-Rich Fluid Activity along a Subduction Interface in the Paleoproterozoic Wutai Complex, North China Craton B. Wang et al. 10.3390/min11070748
- Zircon U-Pb and geochemical signatures in high-pressure, low-temperature metamorphic rocks as recorders of subduction zone processes, Sikinos and Ios islands, Greece E. Poulaki et al. 10.1016/j.chemgeo.2021.120447
- Rheology modification in a subduction channel due to eclogite facies metasomatism (Rocky Beach Metamorphic Mélange, Port Macquarie, Australia) M. Finch et al. 10.1016/j.lithos.2024.107797
- A review of the geochemical changes occurring during metamorphic devolatilization of metasedimentary rocks A. Stepanov 10.1016/j.chemgeo.2021.120080
1 citations as recorded by crossref.
Latest update: 10 Dec 2024
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...
