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 Typically, is in the range 0.8–1.5, but for the Chi–Chi earthquake the value is = 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. 其他題名： Pure Appl. Geophys 出版者： Basel: SP Birkhäuser Verlag Basel 出版日期： 2013-01 出處： Pure and applied geophysics, 2013-01, Vol.170 (1-2), p.221-228 資源來源： Agricultural & Environmental Science Collection 版權： Springer Basel AG 2012 版權： Springer Basel 2013 識別號： ISSN: 0033-4553 識別號： EISSN: 1420-9136 識別號： DOI: 10.1007/s00024-011-0445-5
