<b>Nature and genesis of post-collisional potassic volcanic rocks in the western Kunlun, NW Tibetan Plateau: Implication for the recycling of</b> <b>carbonate-bearing sediments</b>

Table S1 major (wt.%) and trace element (ppm) compositions of reference materials and trace element compositions of blank (ppb)Table S2 Sr–Nd–Pb isotopic compositions of reference materialsTable S3. Whole-rock major (wt.%) and trace element (ppm) data for post-collisional potassic volcanic rocks in the western Kunlun, NW Tibetan PlateauTable S4. Whole-rock Sr-Nd-Pb isotopic compositions for post-collisional potassic volcanic rocks in the western Kunlun, NW Tibetan PlateauTable S5. Whole-rock Mg isotopic compositions for post-collisional potassic volcanic rocks in the western Kunlun, NW Tibetan PlateauTable S6. Parameters used for non-modal batch partial melting model.<br>