Analysis reveals zircon U-Pb dating and isotopic results from bimodal magmatic rocks, suggesting insights into the evolution of the Karamaili Ocean.
Table S1: Locations of zircon U-Pb dating samples from the early Silurian bimodal magmatic rocks from the northeastern Junggar block. Table S2: Zircon U-Pb analytical results for the early Silurian bimodal magmatic rocks from the northeastern Junggar block. Table S3: Zircon Hf isotopic results for the early Silurian bimodal magmatic rocks from the northeastern Junggar block. Table S4: Whole-rock major and trace element compositions for the early Silurian bimodal magmatic rocks from the northeastern Junggar block.
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Huang et al. (2025) studied this question.
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