The Beijie gold deposit in Zhaoyuan city is one of the earliest discovered gold deposit in the northwest Jiaodong area. It is a typical altered tectonite type gold deposit which lies in beresitization alteration zone strictly controlled by an NEE fault. This article studies geological background and zircon SHRIMP geochronology of diorite porphyrite cutting through orebody and Beijie intrusion from Guojialing sequences. Dating result of zircons from diorite porphyrite is 117±2Ma and Beijie intrusion is 129±1Ma, suggesting that the Beijie gold deposit was formed in early Cretaceous with an age of 117~129Ma. Multiple stages of inherited zircon age of Ar3,Z,J3 gained from zircons in Beijie intrusion and diorite porphyrite imply that the process of rock forming was very complicated and inherited. Guojialing sequence is 5~10Ma earlier than gold deposits in the Jiaodong area, and it is more closer to gold deposits in space distribution, suggesting that it is much more closer to a magma source of ore forming fluid in the Jiaodong area. Ore forming stage and tectonic environment of Jiaodong gold deposits are also discussed. It is conclucled that the Jiaodong gold concentration area was formed in an environment of back arc extending. Its formation and evolution were controlled by large scale lithospheric thinning, mantle upwelling, and continental margin rift in east China in Mesozoic. It was very probably related to a mantle plume.