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In this paper,the Gaoyou-Baoying M_S4.9 earthquake was analyzed by the geomagnetic harmonic wave amplitude ratios method. The earthquake was an isolated seismic event,before and after which there were no other earthquakes occurred in this region. The dense distribution of geomagnetic observataries provided an advantage condition for the analysis of characteristics of the geomagnetic harmonic amplitude ratios. The analysis results verify the former knowledge of anomaly characteristics of the geomagnetic harmonic amplitude ratio,that is,the anomalous characteristics of the earthquake mostly appeared during the decline-turning-recovery rising process. The results also show that the change of the anomalies was asynchronous at the observatories close to the epicenter, namely, the anomalous characteristics were different between the H and the D components,as well as between the long and short periods.
The earthquake was an isolated seismic event, before and after which there were no other earthquakes occurred in this region. The dense distribution of geomagnetic The analysis results verify the former knowledge of anomaly characteristics of the geomagnetic harmonic amplitude ratio, that is, the anomalous characteristics of the earthquake mostly The results also show that the change of the anomalies was brief at the observatories close to the epicenter, namely, the anomalous characteristics were different between the H and the D components, as well as between the long and short periods.