August 6, 2025

Supplemental Material: Carbonation of oceanic serpentinite related to extensive intraplate magmatism

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MAIN FINDING: Carbonation of oceanic serpentinite is significantly influenced by intraplate magmatism processes.
KEY EVIDENCE: Data indicates a strong relationship between magmatic activity and serpentinite carbonation rates.
APPROACH: Analysis involved geological samples and techniques to assess carbonation and magmatism interconnectivity.
SIGNIFICANCE: Understanding this relationship enhances knowledge of geological carbon storage and tectonic processes.

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Research reveals carbonation processes in oceanic serpentinite due to intraplate magmatism, suggesting geological implications.

Supplemental Text S1, Figures S1–S3, and Tables S1–S7.

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Oyanagi et al. (2025) studied this question.

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Research reveals carbonation processes in oceanic serpentinite due to intraplate magmatism, suggesting geological implications.

Supplemental Text S1, Figures S1–S3, and Tables S1–S7.