矿物的裂变径迹年龄分析可有效地用于热液矿床成矿时代的研究。对金顶超大型铅锌矿床的成矿年龄存在不同的看法，本文以架崖山矿段为代表，采用磷灰石裂变径迹分析方法测定了金顶铅锌矿床的成矿年龄。结果表明：金顶铅锌矿床的成矿期在渐新世，其后遭受了喜马拉雅造山运动的热扰动。 Fission track age analysis of minerals can be effectively used in hydrothermal mineralization research. There are different opinions on the metallogenic age of the Jinding ultra-large lead-zinc deposit. In this paper, the Mount Yiaoshan deposit is represented by the apatite fission track analysis method to determine the metallogenic age of the Jinding Pb-Zn deposit. The results show that the metallogenic stage of the Jinding Pb-Zn deposit is Oligocene, and then suffered thermal disturbance from the Himalayan orogeny.