<b>Reversed Fe-Zn isotopes reveal pervasive hydration and fluid-driven element exchange in oceanic lithospheric mantle</b>

Table S1 Fe and Zn isotope compositions of olivine (Ol), orthopyroxene (Opx), spinel (Sp), and clinopyroxene (Cpx) in lherzolites, harzburgites, dunites, and chromitites from Purang ophiolite