Supplemental Text S1: Analytical methods; Figure S1: Plots of variation of selected trace elements vs. Zr to check for element mobility during postmagmatic alteration; Table S1: Zircon U-Pb data sources for Paleozoic to early Mesozoic intrusive rocks in central Inner Mongolia; Tables S2 and S3: Whole-rock major-element and trace-element geochemistry, and Sr-Nd isotopic compositions; Tables S4 and S5: Zircon U-Pb-Hf isotopic data; Table S6: EPMA results of amphibole from the late Carboniferous Mandula intermediate to acidic composite pluton; and Table S7: Summary of crustal thickness calculation in central Inner Mongolia.
No takes yet. Share an insight, caveat, or question.
Gao et al. (2024) studied this question.
Synapse has enriched one closely related paper. Consider it for comparative context: