《Table 3 Zircon Lu-Hf isotopic compositions of olivine websterite in the No.I mafic-ultramafic compl

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《"Geochronology, Geochemistry and Sr-Nd-Pb-Hf Isotopes of No. I Complex from the Shitoukengde Ni–Cu Sulfide Deposit in the Eastern Kunlun Orogen, Western China: Implications for the Magmatic Source, Geodynamic Setting and Genesis"》

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Zircons were separated from whole-rock samples using the conventional heavy liquid and magnetic techniques，and then by handpicking under a binocular microscope，at the Langfang Regional Geological Survey，Hebei Province，China.The handpicked zircons were examined under transmitted and reflected light with an opticalmicroscope.To reveal their internal structures，cathodoluminescence（CL）images were obtained using a JEOL scanning electron microscope housed at the State Key Laboratory of Geological Processes and Mineral Resources，China University of Geosciences，Wuhan，China.The testing method，testing process and data processing are introduced in reference of Tang et al.（2015）and the data are shown in Table 1.