August 15, 2025Open Access

Supplemental Material: Fe isotope decoding of fluid-absent versus fluid-present melting of deeply subducted continental crust

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Fluid-absent melting occurs at higher temperatures compared to fluid-present conditions in subducted continental crust, indicating a significant thermal influence.
The study provides detailed modeling calculations that illustrate how Fe isotopes can decode the melting processes, highlighting critical geological insights.
Employing advanced geochemical analysis techniques, this research explores the melting conditions of deeply subducted continental crust affected by fluids.
Findings suggest that fluids play a crucial role in melting mechanisms, which may have implications for understanding volcanic activity and crustal evolution.

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Modeling reveals differences in fluid-absent and fluid-present melting of subducted continental crust, suggesting insights into geological processes.

Methodology, detailed modeling calculations, Figures S1–S9, and Tables S1–S3.

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Zhu et al. (2025) studied this question.

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Modeling reveals differences in fluid-absent and fluid-present melting of subducted continental crust, suggesting insights into geological processes.

Methodology, detailed modeling calculations, Figures S1–S9, and Tables S1–S3.