Based on stratigraphic data from geothermal deep wells, a geological profile was plotted across the Huangzhuang-Gaoliying fault zone, and deep tectonic characteristics are discussed. Combined with existing data, research results showed that at least four transformations of the normal and reverse faults, with features of repeated concussion, occurred along the Huangzhuang-Gaoliying fault. It is held that the cause of the fault was the fracture of a regional plate, with subsequent, frequent horizontal movement of the plate changing many times, resulting in repeated transformations in tension and compression. Decline and thrusting motion of the hanging wall constantly occurred, also exhibiting features of repeated concussion. Formation age of the fault was about 106-140 million years b.p., which was late Jurassic (J₃). The later rock activity produced local extrusion and uplift, which restricted the activities of the south and north ends of the hanging wall, resulting in the phenomenon of uplift and tilt at one end. While movement of the middle segment of the upper plate was relatively more free, the average decline rate was about 3 mm per year. Based on analysis of the structural features and historical seismic records, it is suggested that the monitoring of this activity should focus on the horizontal movement of plates at both sides of the fault zone.