This analysis reveals two-stage northward subduction in the Tibetan Plateau, implying complex geological processes.
Text S1: Analytical methods. Tables S1–S3: LA-ICP-MS zircon U-Pb, trace-element, and Lu-Hf isotopic data for the sandstone and andesite samples of the central Tibetan Plateau. Table S4: Whole-rock major- and trace-element compositions of the Jurassic andesite and basalt samples.
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Liu et al. (2025) studied this question.
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