Supplemental Material: Oceanic subduction to continental collision in the NE Proto- Tethys revealed by early Paleozoic eclogites with high temperature granulite-facies overprinting in the East Kunlun orogenic belt, northern Tibet

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Text: Analytical methods. Table S1: Representative electron microprobe analyses of garnet in eclogite samples. Table S2: Representative analyses of clinopyroxene (omphacite) in eclogite samples. Table S3: Representative microprobe analyses of low-sodic clinopyroxene in eclogite samples. Table S4: Representative microprobe analyses of amphibole in eclogite samples. Table S5: Representative microprobe analyses of plagioclase in eclogite samples. Table S6: Representative microprobe analyses of other minerals (orthopyroxene and epidote) in eclogite samples. Table S7: Whole-rock major (wt%) and trace element (ppm) analyses of eclogites in Nuomuhong area, East Kunlun orogenic belt. Table S8: SHRIMP Zircon U–Pb isotopic data from the eclogite in Nuomuhong area, East Kunlun orogenic belt. Table S9: Rare earth elements (ppm) analyses of the tested zircons from the retrograde eclogites.