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Garnet zoning patterns record multiple processes of chemical transfer during subduction

George, Freya R.; Viete, Daniel R.; Ávila, Janaína; Seward, Gareth G.E.; Guice, George L.; Allen, Mark B.; Harrower, Michael J.

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Authors

Freya R. George

Daniel R. Viete

Janaína Ávila

Gareth G.E. Seward

George L. Guice

Michael J. Harrower



Abstract

Subduction is the principal mechanism by which volatiles are transferred from the Earth's surface to its interior. In garnets from eclogites and blueschists formed within the subduction setting, fine-scale, oscillatory elemental zoning is a common feature, sometimes considered to record open-system fluid exchange during prograde metamorphism. We present oxygen isotope data for garnets with such zoning from five exhumed subduction zone complexes. Short length scale fluctuations in elemental and oxygen isotope zoning (which are themselves spatially decoupled) cannot be linked to open-system fluid exchange during garnet crystallization in all samples; these data do not provide evidence for a genetic relationship between elemental oscillations and fluid fluxing. However, garnets from one setting do provide clear evidence for syn-growth ingress of elementally and isotopically buffering fluids, a process that operated simultaneously with the formation of elemental oscillations. Our findings indicate multiple mechanisms of chemical transfer operate at the grain–rock scale during subduction, and that some subduction zone rocks may experience only limited interaction with external prograde fluids. These results are consistent with a picture of highly heterogenous volatile transfer during subduction, and suggest that some proportion of the fluid inventory inherited at shallow depths may be transferred to sub-arc depths.

Citation

George, F. R., Viete, D. R., Ávila, J., Seward, G. G., Guice, G. L., Allen, M. B., & Harrower, M. J. (2024). Garnet zoning patterns record multiple processes of chemical transfer during subduction. Earth and Planetary Science Letters, 631, Article 118634. https://doi.org/10.1016/j.epsl.2024.118634

Journal Article Type Article
Acceptance Date Feb 23, 2024
Online Publication Date Mar 2, 2024
Publication Date 2024-04
Deposit Date May 22, 2024
Publicly Available Date May 22, 2024
Journal Earth and Planetary Science Letters
Print ISSN 0012-821X
Electronic ISSN 1385-013X
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 631
Article Number 118634
DOI https://doi.org/10.1016/j.epsl.2024.118634
Public URL https://durham-repository.worktribe.com/output/2456113

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