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

Abstract

<p>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.</p>