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

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Figshare2022-11-09 更新2026-04-08 收录
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<strong>Supplementary Text</strong> <strong>S1: </strong>Detailed sample descriptions, analytical methods, and results. <strong>Table S1: </strong>U-Pb dating and REE data of detrital zircons from the Gangdese Mountains, southern Tibet. <strong>Table S2: </strong>U-Pb dating and REE data of detrital zircons from Earth’s major rivers. <strong>Table S3: </strong>Summary of detrital zircon data compiled for the comparison of the Lhasa terrane and its potential origins in Gondwana. <strong>Table S4: </strong>Summary of age, geochemical, and isotopic data of typical Precambrian to Early Paleozoic magmatic rocks in the Lhasa terrane. <strong>Table S5: </strong>U-Pb dating, Hf-isotope, and REE data of detrital zircons from the Lhasa terrane. <strong>Table S6: </strong>U-Pb dating and Hf-isotope data of zircons from typical Precambrian to Early Paleozoic magmatic rocks in the Lhasa terrane. <strong>Table S7: </strong>U-Pb dating, Hf-isotope, and REE data of detrital zircons from Africa. <strong>Table S8: </strong>U-Pb dating, Hf-isotope, and REE data of detrital zircons from India. <strong>Table S9: </strong>U-Pb dating, Hf-isotope, and REE data of detrital zircons from Australia. <strong>Table S10: </strong>U-Pb age, Hf-isotope, and REE analysis results of standard zircons. <strong>Figure S1:</strong> 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). <strong>Figure S2:</strong> Photographs and photomicrographs of the Precambrian to early Paleozoic sedimentary rocks and granitic intrusions in the Lhasa terrane. <strong>Figure S3:</strong> Concordia plots and typical cathodoluminescence images of zircons from the magmatic rock samples analyzed in this study. <strong>Figure S4:</strong> Concordia plots and typical cathodoluminescence images of detrital zircons from the samples analyzed in this study. <strong>Figure S5:</strong> 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. <strong>Figure S6:</strong> 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.
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Hu, Peiyuan
创建时间:
2022-11-09
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