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