Supplemental Material: Termination of the Paleo-Asian Ocean in the Beishan orogen, NW China: Constraints from detrital zircon U-Pb age and Hf isotope analysis of turbidites

Abstract

<p>Table S1: LA-ICP-MS data for the Permian turbidites in southern Beishan, China. Table S2: Zircon Lu-Hf isotopic analyses from the Permian turbidites in southern Beishan, NW China. Table S3: Sr-Nd isotopic data for the Permian turbidites in southern Beishan. Figure S1: Compound U-Pb concordia diagrams of samples collected from Permian turbidites in the southmost Beishan orogenic collage. Figure S2: Compound U-Pb concordia diagrams of Paleozoic detrital zircons in this study. Figure S3: Age histograms and relative probability diagrams of detrital zircons from every single sample. Figure S4: Comparison of age histograms and relative probability plots for detrital zircons U-Pb ages of Paleozoic sedimentary rocks in Southern Altaids.</p>