Supporting-Information - Text of Tectonic burial of sedimentary rocks drives the building of juvenile crust of magmatic arc

Text S1 describes the analytical methods used in this study. Figure S1 is the X-ray mappings of garnets from the pelitic migmatites. Table S1 is the chemical compositions of garnet from the studied pelitic migmatites. Table S2 is representative chemical compositions of other minerals from the pelitic migmatites. Table S3 shows the whole rock Sr–Nd isotopes and major element compositions of the studied pelitic migmatite, the Late Cretaceous arc magmatic rocks and Neo-Tethyan ophiolites. Table S4 is zircon U–Pb dating and trace element data. Table S5 shows the zircon Lu–Hf and oxygen isotopic data.