## 摘要

In this paper we consider the statistics of the aftershock sequence of the m = 7. 65 20 September 1999 Chi-Chi, Taiwan earthquake. We first consider the frequency-magnitude statistics. We find good agreement with Gutenberg-Richter scaling but find that the aftershock level is anomalously high. This level is quantified using the difference in magnitude between the main shock and the largest inferred aftershock δm^{*}: Typically, δm^{*} is in the range 0.8-1.5, but for the Chi-Chi earthquake the value is δm^{*} = 0.03. We suggest that this may be due to an aseismic slow-earthquake component of rupture. We next consider the decay rate of aftershock activity following the earthquake. The rates are well approximated by the modified Omori's law. We show that the distribution of interoccurrence times between aftershocks follow a nonhomogeneous Poisson process. We introduce the concept of Omori times to study the merging of the aftershock activity with the background seismicity. The Omori time is defined to be the mean interoccurrence time over a fixed number of aftershocks.

原文 | ???core.languages.en_GB??? |
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頁（從 - 到） | 221-228 |

頁數 | 8 |

期刊 | Pure and Applied Geophysics |

卷 | 170 |

發行號 | 1-2 |

DOIs | |

出版狀態 | 已出版 - 1月 2013 |