沿消减带的某些板块边界似乎长期无震。
Certain parts of the plate boundaries along subduction zones appear to be aseismic.
并认为无震异常空间分布的不均匀性、时间分布上的突发性特征与此有关。
It is held that this is responsible to the inhomogeneity of the space distribution of aseismic anomalies and the jump of the time distribution.
并与研究区内随机挑选的25个无震子区的构造因子进行了综合类比分析。
A synthetic study of analogy has been made by using the structural factors between these structure backgrounds and 25 aseismic sub-areas selected randomly from the studied region.
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