 The beta geostationary satellites are capable of detecting changes in the ionosphere's total electron content, TEC. These changes can be measured using distinct horizontal azimuths and elevation angles, allowing for the detection of TEC perturbations caused by the minuant earthquake. The TEC perturbations were found to travel away from the epicenter at speeds of 800 meters per second and 1000 meters per second. This study demonstrates the potential of geostationary satellites as a tool for monitoring TEC changes. This article was authored by Fei Wang, Xu Amin Zhang, Lei Dong, and others.