Supplemental Material: Geochemical and petrological diversity of a transcrustal magmatic system driven by mushy magma mixing: Insights from the Triassic dike swarms in East Kunlun orogen, northern Tibetan Plateau

Text S1: Analytical methods. Figure S1: Representative cathodoluminescence images of zircons and U-Pb concordia diagrams for the studied dike swarms in the East Kunlun orogenic belt, northern Tibetan Plateau. Table S1: Whole-rock major- and trace-element compositions of the studied Triassic dike swarms in the East Kunlun orogenic belt, northern Tibetan Plateau. Table S2: LA-ICP-MS zircon U-Pb data for the studied Triassic dike swarms in the East Kunlun orogenic belt, northern Tibetan Plateau. Table S3: Major-element compositions of minerals for the studied Triassic dike swarms in the East Kunlun orogenic belt, northern Tibetan Plateau. Table S4: Trace-element compositions of minerals for the studied Triassic dike swarms in the East Kunlun orogenic belt, northern Tibetan Plateau. Table S5: Whole-rock Sr-Nd isotopic compositions for the studied Triassic dike swarms in the East Kunlun orogenic belt, northern Tibetan Plateau. Table S6: Zircon Lu-Hf isotopes for the studied Triassic dike swarms in the East Kunlun orogenic belt, northern Tibetan Plateau.