希腊Ionian海Kefallinia转换断裂带的地震复发行为
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摘要
采用历史地震资料和统计方法研究了希腊Ionian海Kefallinia转换断裂带的两条断层(Kefallinia和Lefkada)的整体强地震复发行为。研究发现,Kefallinia断层的地震复发行为表现出丛集性特征,存在时间可预测复发行为;Lefkada断层的地震复发行为具有近随机性特征,不存在时间可预测及滑动可预测的复发行为。造成其地震复发行为不同的原因可能有:(a)沿Kefallinia断裂带走向,由静力触发引起的断层分段间的相互作用;(b)Lefkada断层的地震复发行为受北部和东部的断层系影响。另外,活跃期内地震复发间隔分布的分散性较大,可用韦伯( Weibull)分布近似描述;而平静期持续时间分布的分散性不够,这样的分布不便进行拟合。
We examined the whole strong earthquake recurrence behaviors of two fault zones along the Kefallinia Transform, Ionian Sea, Greece, using seismological data and statistical methods. We found different recurrence behaviors for the Kefallinia Fault Zone (clustering and time-predictable recurrence behaviors) and the Lefkada Fault Zone (near random and non-slip-predictable or non-time-predictable recurrence nature). The different modes may be attributed to: (a) segment interaction along-strike (Kefallinia) by static triggering and (b) the influence of fault systems to the north and east on the recurrence on Lefkada. Within the active periods, earthquake recurrence intervals are distributed in a more dispersed fashion, and can be fitted well by a Weibull distribution. In contrast, the distribution of the quiet periods is relatively less dispersed and difficult to describe by suitable probability functions.
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