Data for sulfur isotopes from the lunar farside reveal a global evaporation signiture following the gaint impact

Table S1. Mineral composition of clinopyroxene and plagioclase in CE-6 basalt and crustal clasts.Table 2. Mineral abundance of CE-6 basalt clasts, NWA 12008 and NWA 14526 analysed by TIMA.Table S3. Composition of sulfide in Chang'e-6 basalt clasts, highland clasts and breccias.Table S4. δ34SV-CDT value of troilites in CE-6 basalt clasts, breccias and highland clasts, and lunar meteorites NWA 14526 and NWA 12008.Table S5. 34SV-CDT value of reference materials.