Reversed inter-mineral Fe-Zn isotope fractionation in ophiolitic peridotites: Evidence for widespread hydration of oceanic lithospheric mantle

Published: 10 April 2026| Version 1 | DOI: 10.17632/y6sz2n5tys.1
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Benxun Su

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Supplementary materials for “Reversed inter-mineral Fe-Zn isotope fractionation in ophiolitic peridotites: Evidence for widespread hydration of oceanic lithospheric mantle”

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