August 6, 2025

Supplemental Material: Recycling of carbonated sediments into the mantle: Insights from Li-Mg-Zn isotopes of mafic rocks in the eastern North China Craton, China

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MAIN FINDING: Li-Mg-Zn isotopes indicate carbonated sediments are recycled into the mantle.
KEY EVIDENCE: Isotope analysis of mafic rocks from the North China Craton supports these findings.
APPROACH: The research utilized isotopic techniques to study the geological history of the area.
SIGNIFICANCE: Understanding sediment recycling contributes to knowledge of mantle dynamics and rock formation processes.

Implication

Analysis reveals Li-Mg-Zn isotopes in mafic rocks from the North China Craton, suggesting sediment recycling into the mantle.

Figures S1–S8, Text S1, and Tables S1–S11: Additional information regarding analytical methods and results.

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Yan et al. (2025) studied this question.

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Analysis reveals Li-Mg-Zn isotopes in mafic rocks from the North China Craton, suggesting sediment recycling into the mantle.

Figures S1–S8, Text S1, and Tables S1–S11: Additional information regarding analytical methods and results.