Abstract:Nine DC apparent resistivity stations within a 300km radius of the Jishishan MS 6.2 earthquake,which occurred on December 18,2023,were in normal operation. Among these,five stations provided high-quality data,while the remaining four were rendered ineffective due to environmental disturbances in the monitoring areas. Notably,anomalous variations at the Dingxi station were first observed in June 2021 and have persisted without recovery following the Menyuan MS6.9 earthquake in January 2022. Since June 2023,both the Wushengyi and Wuwei stations have exhibited declining anomalous trends,while the Wudu station,located 335km from the epicenter,has shown an upward trend during the same period. Based on the anomalies recorded at these four stations,a potential risk of a magnitude 6 earthquake was identified within the region spanning the eastern section of the Qilian Mountain seismic belt to southeastern Gansu Province. The anticipated focal mechanism was predominantly of the thrust type. Furthermore,following the emergence of short-term anomalous variations at the Tongwei station in October 2023,a short-term seismic forecast was presented during the weekly earthquake situation meeting on October 27. Subsequently,the Jishishan MS6.2 earthquake on December 18 occurred within the predicted region,and its focal mechanism solution confirmed a thrust-type event.