Slab-controlled progressive evolution of the Kudi back-arc ophiolite in response to the rollback of the Proto-Tethys oceanic slab, in Western Kunlun, NW Tibet Plateau

<b>Table S1 </b>Zircon U-Pb ages of three Kudi ophiolite samples.<br> <b>Table S2 </b>Results of zircons Hf isotope compositions of samples. <b>Table S3</b> Results of whole-rock major (wt.%) and trace (ppm) data on the Kudi ophiolite. <b>Table S4 </b>Results of the whole-rock Sr-Nd-B isotope compositions of the Kudi ophiolite. <b> </b> <b>Table S5 </b>Major elements of olivine from the Kudi ophiolite. <b>Table S6 </b>Major elements of spinel from the Kudi ophiolite. <b>Table S7 </b>Major elements of amphibole from the Kudi ophiolite.