TableS1-S10, Figure S1-S6, and Supplementary text for detrital zircons from northern Gondwana (20221109)

Supplementary Text S1: Detailed sample descriptions, analytical methods, and results. Table S1: U-Pb dating and REE data of detrital zircons from the Gangdese Mountains, southern Tibet. Table S2: U-Pb dating and REE data of detrital zircons from Earth’s major rivers. Table S3: Summary of detrital zircon data compiled for the comparison of the Lhasa terrane and its potential origins in Gondwana. Table S4: Summary of age, geochemical, and isotopic data of typical Precambrian to Early Paleozoic magmatic rocks in the Lhasa terrane. Table S5: U-Pb dating, Hf-isotope, and REE data of detrital zircons from the Lhasa terrane. Table S6: U-Pb dating and Hf-isotope data of zircons from typical Precambrian to Early Paleozoic magmatic rocks in the Lhasa terrane. Table S7: U-Pb dating, Hf-isotope, and REE data of detrital zircons from Africa. Table S8: U-Pb dating, Hf-isotope, and REE data of detrital zircons from India. Table S9: U-Pb dating, Hf-isotope, and REE data of detrital zircons from Australia. Table S10: U-Pb age, Hf-isotope, and REE analysis results of standard zircons. Figure S1: Plots of REE vs. U-Pb ages, age distribution histograms, and plots of REE averages for the detrital zircons from the Earth’s major rivers (A and B) and Gangdese Mountains (C and D). Figure S2: Photographs and photomicrographs of the Precambrian to early Paleozoic sedimentary rocks and granitic intrusions in the Lhasa terrane. Figure S3: Concordia plots and typical cathodoluminescence images of zircons from the magmatic rock samples analyzed in this study. Figure S4: Concordia plots and typical cathodoluminescence images of detrital zircons from the samples analyzed in this study. Figure S5: Plots of LREE/HREE vs. U-Pb ages, age distribution histograms, and plots of LREE/HREE averages for the detrital zircons from the Lhasa terrane and its potential origins in Gondwana. Figure S6: Plots of Eu/Eu* vs. U-Pb ages, age distribution histograms, and plots of Eu/Eu* averages for the detrital zircons from the Lhasa terrane and its potential origins in Gondwana.