摘要
Precursory anomalies of deformation and fluid measured in fixed-point appear the trend features of moving and concentrating from distance areas to the near of seismic area before the Zhangbei MS6.2 earthquake in 1998. Constructing abnormal signal spreading function,and using grid searching-quasi Newton least square method, the authors inverse the converged region of precursory anomalies which is the predicting possible risk region. The result shows that the distance between the margin of calculated converged region and the real epicenter is only 25~51 km. The difference between the converging time and the original time is only several days. Moreover, the converging rate speeds up at the middle-short term before Zhangbei MS6.2 earthquake.