《Table 3 Zircon LA-ICPMS U-Pb isotopic compositions of rocks from the Paodaoling area》

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《"Mineralization, Geochemistry and Zircon U-Pb Ages of the Paodaoling Porphyry Gold Deposit in the Guichi Region, Lower Yangtze Metallogenic Belt, Eastern China"》

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The results of the zircon trace elements are listed in Table 4.All zircons show typical LREE depletions and HREE enrichments with positive Ce and negative Eu anomalies（Fig.13）.Total zircon REE contents for both the Paodaoling and Wushi porphyries range from 350 to1200 ppm，whereas those for both the Huayuangong granites and Wushi quartz-syenites are from 1800 to 4400ppm.Zircons from the Wushi quartz-syenites also show LREE enrichments，suggesting that the zircons may have been contaminated by LREE-enriched minerals（e.g.，apatite）or inclusions（Wang et al.，2014）.