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

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.附表S1：参考标准物质的主量元素（质量分数，wt.%）与微量元素（ppm）组成，以及空白样的微量元素含量（ppb）；附表S2：参考标准物质的Sr–Nd–Pb同位素组成；附表S3：青藏高原西北部西昆仑地区碰撞后钾质火山岩的全岩主量元素（wt.%）与微量元素（ppm）数据；附表S4：青藏高原西北部西昆仑地区碰撞后钾质火山岩的全岩Sr-Nd-Pb同位素组成；附表S5：青藏高原西北部西昆仑地区碰撞后钾质火山岩的全岩Mg同位素组成；附表S6：非模态批式部分熔融模型所用参数。