Mo isotope evidence for the significance of subducted continental crust in formation of post-collisional porphyry Cu deposits

Text S1 is the detailed analytical methods for zircon SIMS U–Pb dating and oxygen isotopes, and whole-rock major and trace elements and Sr–Nd isotopes. Tables S1 to S4 are the analytical results for the above items. Tables S5 shows the whole-rock Mo isotope data. Table S6 is the parameters for geochemical modeling. Figures S1 to S2 are the supplementary diagrams to evaluate the effects of shallow processes on the Mo isotope compositions. Figure S3 shows the Cu contents of the high-Mg diorites and potassic to ultrapotassic rocks from eastern Gangdese and western Lhasa.