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. Our data include 29 events with M ...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. Our data include 29 events with M 〉 5.5 for the period 1636 - 2003. We found different recurrence behaviors for the Kefallinia Fault Zone （clustering and time-predictable recurrence behaviors） and the Letkada 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.展开更多
基金This paper is part result of the program"Investigation of recurrence modes of large earthquakes alongthe main seismogenic faults in Greece andin China"(20051696) in the frame of bilateral cooperation between China and Greece inthefield of seismology and geophysics sponsored bythe Ministry of Science and Technologyof China This programis mainlyfunded bythe NSF40674024 and the NSF40374019
文摘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. Our data include 29 events with M 〉 5.5 for the period 1636 - 2003. We found different recurrence behaviors for the Kefallinia Fault Zone （clustering and time-predictable recurrence behaviors） and the Letkada 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.
