Based on a systematic petrographic and geochemical study and a zircon UPb SHRIMP age analysis, the authors revealed that the age of orehosting volcanics (XC011 rhyolitic tuff) is 180.4±3.5 Ma. This age suggests that the volcanic suite was formed in Early Jurassic instead of formerly widelyaccepted Late Cretaceous. The age of peripheral monzonitic granite (XTM041) is 46.6±0.6 Ma, implying that this granite suite was formed in the oreforming stage of Eocene. According to these data, the authors tend to believe that the Xiongcun superlarge deposit belongs probably to the altered cataclastite type CuAu deposit, and is very similar to Jiaodong “Jiaojiastyle” gold deposits.