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First direct evidence of the O–H isotopic composition of slab-derived water in the subduction zone, revealed by fluid inclusions in high-pressure metamorphic rocks

Crossref DOI link: https://doi.org/10.1186/s40562-025-00396-4

Published Online: 2025-05-02

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Yoshida, Kenta K.

Uemura, Ryu

Ijiri, Akira

Ikehara, Minoru

Hirajima, Takao
Funding

Funding for this research was provided by:

Japan Society for the Promotion of Science (JP13J00057, JP19K14825, JP22H00171, and JP23H03814, JP20H00628, JP22H05308, JP25257208, JP19H01999, and JP21109004)
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Article History

Received: 27 February 2025

Accepted: 23 April 2025

First Online: 2 May 2025

Declarations

:

: The authors declare no competing interests.

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