Supplemental Material: Ediacaran magmatism and rifting along the northern margin of the Tarim craton: Implications for the late Neoproterozoic Rodinia configuration and breakup

Table S1: Detail analytical methods. Table S2: Analytical results of major- and trace-element compositions of the Lower Ediacaran Sugetbrak basalts in the northwest Tarim craton. Table S3: Analytical results of Sr-Nd-Hf-Pb isotope compositions of the Lower Ediacaran Sugetbrak basalts in the northwest Tarim craton. Table S4: Laser-ablation–inductively coupled plasma–mass spectrometry (LA-ICP-MS) U-Pb data for detrital zircons in the Sugetbrak Formation sandstones. Table S5: Compilation of zircon U-Pb dating data for the magmatic rocks from the Central Tianshan terrane. Figure S1: Cathodoluminescence (CL) images of representative zircons with analyzed spots and preferred ages (in Ma). Figure S2: Detrital zircon Th/U ratio vs. age plot for two sandstone samples in this study.