The seismic exploration was used to explore the potential geothermal resource and geological structure in Xian County, N China. Micro-logging was used to conduct surveys on the velocity structure near the surface, the static correction models and the observation system was determined by this method. By testing different borehole depths and different quantities of explosives, the best experimental parameters were obtained in a series of test locations and in two test sections. The surface differences were eliminated by the static correction, and an interference wave survey was conducted to improve the data signal to noise ratio (SNR). The post-stack wave equation for the PR splitting finite difference was used for migration imagery, and post-stack, underground imaging profiles were obtained. The corrected seismic signals were then interpreted, and converted into geological information. The results showed that the burial depths and morphology in each layer had been successfully obtained. The areas favorable for heat storage in karst fissures were mainly in the Jixian Formation and the Cambrian–Ordovician. Our investigation allowed us to predict and calibrate favorable locations for two geothermal energy exploration holes.