Whole rock and mineral analysis, and melt compositions of granulites from Grove Mountain, Antarctica

Table S1 Representative chemical compositions of minerals in the UHT granulites from the Grove Mountains, East Antarctica.
Table S2 Effective whole-rock compositions of UHT granulites from the Grove Mountains used in phase equilibria modeling (mol.%).
Table S3 LA-ICP-MS U-Pb isotope and trace element data for zircons of UHT granulites from the Grove Mountains.
Table S4 LA-ICP-MS U-Pb isotope and trace element data for monazites of UHT granulites from the Grove Mountains.
Table S5 LA-ICP-MS in-situ biotite Rb-Sr analysis results for the UHT samples and standard sample ZBH-25.
Figure S1. Melt and garnet content variation diagrams for (a-b) MSW59J-3A2, (c-d) MSW24-1A, and (e-f) MSW22-3A.
Figure S2. T–Xmelt pseudosections for (a) MSW59J-3A2, (b) MSW24-1A, and (c) MSW22-3A. Melt compositions were calculated using the equilibrium conditions of each sample at 1000°C and 7 kbar. Residue compositions were derived by subtracting 35% peak-stage melt compositions from the effective bulk rock compositions for maintaining the H2O content > 0.
Figure S3. Representative zircon cathodoluminescence images for (a) MSW59J-3A2, (b) MSW24-1A, and (c) MSW22-3A. Yellow arrows indicate evidence of melt-mediated coupled dissolution–precipitation replacement reactions.