Supplemental Material: Temporal evolution of the early–late Neoarchean granitoid magmatism in the eastern North China Craton: Transition of geodynamic regime from mantle plume to continental marginal arc system

Abstract

<p>Text S1: Analytical methods. Figure S1: Covariation diagrams of selected elements vs. Zr for whole-rock samples of the granitoids formed during the early and late Neoarchean in the Southern Jilin Province. Table S1: LA-ICP-MS zircon U-Pb analytical data for the different types of granitoids formed during the early and late Neoarchean in the Southern Jilin Province. Table S2: Zircon trace elemental abundances (ppm) for the different types of granitoids formed during the early and late Neoarchean in the Southern Jilin Province. Table S3: Bulk-rock major (wt%) elemental data for the different types of granitoids formed during the early and late Neoarchean in the Southern Jilin Province. Table S4: Bulk-rock trace (ppm) elemental data for the different types of granitoids formed during the early and late Neoarchean in the Southern Jilin Province. Table S5: Zircon Lu-Hf isotopic compositions for the different types of granitoids formed during the early and late Neoarchean in the Southern Jilin Province. Table S6: Whole oxygen isotopes for the different types of granitoids formed during the early and late Neoarchean in the Southern Jilin Province. </p>