Supplementary files: Fertile upper mantle peridotite xenoliths indicate no wholesale destruction of cratonic root in East Asia

Supplementary Data 1–7 captionsSupplementary Data 1: EPMA data: Olivine major element composition (wt%)Supplementary Data 2: EPMA data: Orthopyroxene major element composition (wt%)Supplementary Data 3: EPMA data: Clinopyroxene major element composition (wt%)Supplementary Data 4: EPMA data: Spinel major element composition (wt%)Supplementary Data 5: LA-ICPMS data: REE compositions of clinopyroxene, orthopyroxene, and olivineSupplementary Data 6: LA-ICPMS data: Trace element compositions of clinopyroxene, orthopyroxene, and olivine.Supplementary Data 7: Primitive mantle normalized trace element compositions of clinopyroxene, orthopyroxene, and equilibrium melt compositions (using clinopyroxene) used for plots in supplementary figure 7.Supplementary InformationSupplementary figure 1: Field photographs of xenolith bearing alkali basalt.Supplementary figure 2: Photographs of various xenolith samples used for this study.Supplementary figure 3: Photographs of entire thinsections, and their BSE and Mg composition images.Supplementary figure 4: Optical microscope images of the xenolith samples.Supplementary figure 5: Location of EPMA analysis provided in Supplementary Table 2 are marked in the Mg composition image of each thinsection.Supplementary figure 6: Location of LA-ICPMS analysis provided in Supplementary Table 7 and 8 are marked on the thisection photomicrographs.Supplementary Table 1: Sample locations and other details of samples.Supplementary Table 2: EPMA data: Melt pockets major element composition (wt%)Supplementary Table 3: SIMS data: Oxygen isotope composition of olivine, orthopyroxene, and spinelSupplementary References