A rhyolite porphyry dyke was found in the Zhoujiashan uranium ore deposit from the Xiangshan uranium ore field, which intruded into the porphyroclastic lava in the Xiangshan volcanic complex. LA-ICP-MS zircon U-Pb dating shows that this rock was formed at (134.6±1.2) Ma (MSDW=1.2). In combination with previous studies, the authors concluded that the Xiangshan rhyolite porphyry may have formed in a back-arc extensional setting which related to subduction of the Palaeo-Pacific Plate.