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共搜集到１９７０～１９８４年中亚地区８ 个地震序列。通过分析这些板块内部地震序列的震源分布、震源机制，归纳出它们的特征是：震中分布的长轴都比较短，震中分布长轴和短轴的比值小；长轴的方向受当地地震带的走向控制，和碰撞带走向无关。地震序列中各地震的震源深度都比较浅。其中有震源机制资料的３ 个地震序列表明：主震的震源机制如果是逆冲滑动，倾角则比较低；主震的震源机制如果是走向滑动，倾角则比较高。不论主震的震源机制是倾滑，还是走滑，余震的震源机制和主震的震源机制一致性较差
A total of eight earthquake sequences were collected from 1970 to 1984 in Central Asia. By analyzing the source distribution and focal mechanism of the seismic sequences in these plates, the characteristics of them are summarized as follows: the long axis of the epicenter distribution is relatively short and the ratio of the long axis to the short axis of the epicenter distribution is small; the direction of the long axis is affected by the local seismic band Going to control has nothing to do with the collision zone. Earthquakes in the earthquake focal depths are relatively shallow. Among them, the three earthquake sequences with focal mechanism data show that the focal mechanism of the main shock is relatively low if it is a thrust slip, and the focal mechanism of the main shock is steep and the dip angle is relatively high. Whether the source mechanism of the main shock is dip-slip or slip-off, the focal mechanism of aftershocks is less consistent with the focal mechanism of the main shock