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Supplemental Material: High-temperature altered oceanic crust recycling into oceanic-island basalt–like mantle produces alkaline continental crust driven by mélange diapirs: Insights from isotopic tracing and numerical modeling

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Version 2 2023-07-14, 14:28
Version 1 2023-06-08, 19:45
journal contribution
posted on 2023-07-14, 14:28 authored by Huichuan Liu, Pengpeng Huangfu, et al.

Supplemental Texts S1–S9: Analytical methods. Supplemental Tables S1–S7: Analytical results. Supplemental Figures S1–S5: Supporting figures.

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    GSA Bulletin

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    Keywords

    Altered oceanic crustMélange diapirAlkaline crustCentral Asian Orogenic BeltIsotope tracingNumerical modeling

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    CC BY-NC 4.0

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