Supporting information for the paper entitled "Identification of Miocene olivine leucitites in southern Tibet: Implication for the presence of hidden carbonated mantle reservoir"

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The supporting information provides the evidence for analytical methods (Supplementary text 1); mineral map (a) and photomicrograph (b) of the Maiga olivine leucitites(Supplementary Fig. 1); diagrams of En–Wo–Fs clinopyroxene classification (a) and clinopyroxene O isotopes (b) of the Maiga olivine leucitites (Supplementary Fig. 2); diagrams of (a) CaO (wt.%) versus MgO (wt.%), (b) FeOT/MnO versus MgO (wt.%), and(c) FeOT/CaO-3MgO/SiO2 versus MgO (wt.%) of the Maiga olivine leucitites (Supplementary Fig. 3); Ar-Ar aging data of the Maiga olivineleucitites (Supplementary Table 1); major compositions, O isotopes, and H2O content data of clinopyroxene of the Maiga olivine leucitites (Supplementary Table 2); and whole-rock major-trace elements and Sr-Nd-Pb-Hf-Zn isotope data of the Maiga olivine leucitites (Supplementary Table 3).

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