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研究了我国大陆３７次６级以上地震序列的后续显著地震的时间分布特点及其跟踪预测方法．结果表明：跟踪地震序列应变释放随时间的变化是预测后统显著地震的一个重要途径；而对于超晚期强余震的预测，则需要从区域地震活动性分析着手．
The time distribution features of follow-up significant earthquakes in 37 times of magnitude 6 above earthquakes in China and their tracking methods are studied. The results show that tracking the variation of strain release with time is an important way to predict the significant earthquakes. However, the prediction of strong aftershocks should be based on the analysis of regional seismicity.