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Decoupling of Neogene seawater lithium isotopes from uplift-driven weathering.

Nat Commun · 2026 · PMC13376809 · PMID 42140925

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a decreasing trendno p-value reported
After correcting for the influences of unweathered minerals, the corrected δ 7 Li values of weathering alteration products also exhibit no temporal trend for the Nepal Himalaya and a decreasing trend for the Qaidam Basin during the Neogene (Fig. 2 ).

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