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  • Articles  (2)
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  • 2005-2009  (2)
  • 1980-1984
  • Bulletin of the Seismological Society of America. 2009; 99(2A): 884-891. Published 2009 Apr 01. doi: 10.1785/0120080211.  (1)
  • Bulletin of the Seismological Society of America. 2009; 99(6): 3140-3149. Published 2009 Nov 23. doi: 10.1785/0120080262.  (1)
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  • Articles  (2)
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  • 1
    Publication Date: 2009-11-23
    Description: Maximum seismic intensity maps for Japan are constructed using the recorded intensity data from 1498 to 2007 and are used to test the probabilistic seismic hazard map (PSHM) by the Headquarters for Earthquake Research Promotion, Japan. The historical intensity maps are compared with the hazard maps of probable maximum seismic intensity for a 475-yr return period, assuming a Poisson distribution (10% in 50 yrs). We look at cases that include all events, only subduction zone earthquakes, and all events excluding subduction zone earthquakes. The megathrust earthquakes in the subduction zones produce large bands of high intensities along the Pacific coast side, while onshore crustal earthquakes create a patchy distribution of large intensities over all of Japan. The maximum recorded intensity map for the past 500 yrs and the maximum predicted intensity map for the Formula return period from the PSHM are very similar for the cases including all events and the subduction zone earthquakes, while there is poor correlation for the third category that includes mostly onshore crustal earthquakes. If we consider only the amount of area, not the specific locations, the recorded intensity map and the PSHM (using the maximum case) have a high degree of correlation for Japanese Meteorological Agency (JMA) intensity higher than 4 for all of the cases. Statistically, the present hazard maps for Japan seem to agree with the past intensity distributions and can be regarded as appropriate hazard maps, even though there may be strong dependencies on uncertain model parameters for the PSHMs.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
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  • 2
    Publication Date: 2009-04-01
    Description: We investigate the early aftershock activity associated with four moderate earthquakes (M (sub w) 6.6-6.7) that occurred recently in Japan. For each aftershock sequence, we examine continuous high-pass filtered seismograms recorded at seismic stations nearby the main fault to identify as many early events as possible. The magnitude of these events is calibrated using aftershocks that are listed in the earthquake catalog of Japan Meteorological Agency (JMA). The analysis of the aftershock decay rates reveals a power-law time dependence with a scaling exponent close to 1.0 that starts from about one minute from the mainshock. Our results demonstrate that the c-value of the Omori-Utsu law is very small, although a lower bound is not established due to completeness problems in the first minute after the mainshock and statistical fluctuations.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
    Location Call Number Expected Availability
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