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

<p dir="ltr">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.</p><p><br></p>