The return of stagnant slab recorded by intraplate volcanism.

Proc Natl Acad Sci U S A · 2025 · PMC11725906 · PMID 39793068

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a clear trendno p-value reported

206 Pb/ 204 Pb, the high- 206 Pb/ 204 Pb endmember of Shuangyashan basalts shows a clear trend toward the sediment field rather than the MORB’s scope, suggesting that the source peridotite had been modified by the subducting Pacific sediments ( SI Appendix, Fig.

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