Supplemental Material: New geochronological results from late Mesoproterozoic to early Neoproterozoic successions in the eastern North China Craton and implications for the reconstruction of Rodinia

Figure S1: Cathodoluminescence images of all the analyzed detrital zircon grains from the Penglai Group in this study. Figure S2: Cathodoluminescence images of all the analyzed detrital zircon grains from the Tumen Group in this study. Figure S3: Cathodoluminescence images of all the analyzed detrital zircon grains from the Huaibei Group in this study. Figure S4: Probability density plots of single sample of the Penglai Group in this study. Figure S5: Probability density plots of single sample of the Tumen Group in this study. Figure S6: Probability density plots of single sample of the Huaibei Group in this study. Figure S7: εHf(t) versus age for detrital zircon of the individual sample in this study. Table S1: LA-ICPMS detrital zircon U–Pb dating results. Table S2: MC-LA-ICPMS detrital zircon Lu-Hf isotopic results. Table S3: Detrital zircon U-Pb age summary of the samples from the late Mesoproterozoic to early Neoproterozoic strta in the eastern North China Craton.