Supplemental Material: Within-plate granitoids in the Jiaobei terrane were products of a possible tectonic switch from rifting to subduction collision at ca. 2.1 Ga in the North China craton

Supplemental Text S1: Analytical method. Table S1: Major- and trace-element concentrations of the Dongbaishishan and Gujiacun granitoids. Table S2: LA-ICP-MS U-Th-Pb zircon data of the Dongbaishishan and Gujiacun granitoids. Table S3: Lu-Hf isotopic data of the Dongbaishishan and Gujiacun granitoids. Table S4: Zircon oxygen isotopic data of the Dongbaishishan and Gujiacun granitoids. Table S5: The 2.2–2.1 Ga mafic-felsic magmatism in the North China craton. Table S6: Summary of the spatiotemporal distribution, rock associations, and Hf-Nd isotope characters for G1 and G2 magmatism in the North China craton.