Supplemental Material: Neoproterozoic (ca. 825 Ma) basaltic magmatism in the southeastern margin of the North China Craton and its implications for the configuration of Rodinia breakup

Figures S1–S5, including major element X-ray maps, compositions of plagioclase, Harker diagrams, mineral inclusions and Ti-in zircon temperatures; Tables S1–S6, including mineral major element compositions, bulk rock chemical composition, zircon U-Pb isotopes, zircon trace elements and Lu-Hf isotopes; and analytical methods description.