- 著者
- 
             
             Naoshi Hirata
             
             Shiro Ohmi
             
             Shin'ichi Sakai
             
             Kei Katsumata
             
             Satoshi Matsumoto
             
             Tetsuo Takanami
             
             Akira Yamamoto
             
             Takashi Iidaka
             
             Taku Urabe
             
             Mayumi Sekine
             
             Tooru Ooida
             
             Fumihito Yamazaki
             
             Hiroshi Katao
             
             Yasuhiro Umeda
             
             Masao Nakamura
             
             Norihiko Seto
             
             Takeshi Matsushima
             
             Hiroshi Shimizu
             
             Japanese University Group of the Urgent Joint
             
          
- 出版者
- The Seismological Society of Japan, The Volcanological Society of Japan, The Geodetic Society of Japan
- 雑誌
- Journal of Physics of the Earth (ISSN:00223743)
- 巻号頁・発行日
- vol.44, no.4, pp.317-328, 1996 (Released:2009-04-30)
- 参考文献数
- 21
- 被引用文献数
- 
             
             41
             
             
             43
             
             
          
        
        A disastrous earthquake with a magnitude of 7.2 hit the southern part of Hyogo Prefecture on January 17, 1995. The mainshock was located on an active fault of the Arima-Takatsuki-Rokko fault system. Its focal mechanism was consistent with a right-lateral strike-slip fault trending N40°E. Three days after the occurrence of the mainshock, we started to install a highly dense seismic array in and around the fault area of the quake. Two permanent regional seismic networks of more than 30 stations covered the entire area of 200 km × 200 km. The temporarily installed array of 27 stations spanned the fault area of 15 km × 50 km. All data were telemetered to a temporary observation center at Uji. We located about 3, 100 aftershocks in real time for 1 month using an Internet connection between seismic networks. The aftershock area extended 70 km trending northeast to southwest. Hypocenters determined by the network were delivered automatically through the Internet. We found that the aftershock distribution was heterogeneous in space and time: seven clusters of hypocenters were identified and temporary variation in the rate of occurrence of aftershocks had a periodic component with periods of a half of day, 1 day, and 3 days, that are superimposed on decaying of the rate following Omori's law.