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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

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posted on 2023-07-20, 15:39 authored by Houxiang Shan, et al.

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. 

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