Reversed inter-mineral Fe-Zn isotope fractionation in ophiolitic peridotites: Evidence for widespread hydration of oceanic lithospheric mantle
收藏NIAID Data Ecosystem2026-05-10 收录
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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”
创建时间：
2026-04-10
