Supplemental Material: Late Paleozoic sedimentation recording back-arc basin evolution in response to Chinese Altai–East Junggar convergence in Central Asia

Detrital zircon geochronological data and sandstone framework modal analytical results from this study are included in Supplemental Material Figures S1–S2 and Tables S1–S3. Figure S1: Representative zircon CL images of the analyzed samples from the southern Chinese Altai and northern East Junggar domains. Figure S2: Comparison of the detrital zircon age patterns of the studied sedimentary sequences from the southern Chinese Altai and northern East Junggar domains with the pre-Carboniferous sedimentary rocks from the East Junggar, Chinese Altai, and Mongolian Altai domains. Table S1: Framework modal analytical results of sandstone samples from the southern Chinese Altai and northern East Junggar domains. Table S2: Detrital zircon U-Pb isotopic data of the studied clastic rocks from the southern Chinese Altai and northern East Junggar domains. Table S3: Lu-Hf isotopic compositions of detrital zircons from the strata of the southern Chinese Altai and northern East Junggar domains.