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Possible scenarios for occurrence of M?~?7 interplate earthquakes prior to and following the 2011 Tohoku-Oki earthquake based on numerical simulation.


ABSTRACT: We show possible scenarios for the occurrence of M?~?7 interplate earthquakes prior to and following the M?~?9 earthquake along the Japan Trench, such as the 2011 Tohoku-Oki earthquake. One such M?~?7 earthquake is so-called the Miyagi-ken-Oki earthquake, for which we conducted numerical simulations of earthquake generation cycles by using realistic three-dimensional (3D) geometry of the subducting Pacific Plate. In a number of scenarios, the time interval between the M?~?9 earthquake and the subsequent Miyagi-ken-Oki earthquake was equal to or shorter than the average recurrence interval during the later stage of the M?~?9 earthquake cycle. The scenarios successfully reproduced important characteristics such as the recurrence of M?~?7 earthquakes, coseismic slip distribution, afterslip distribution, the largest foreshock, and the largest aftershock of the 2011 earthquake. Thus, these results suggest that we should prepare for future M?~?7 earthquakes in the Miyagi-ken-Oki segment even though this segment recently experienced large coseismic slip in 2011.

SUBMITTER: Nakata R 

PROVIDER: S-EPMC4861985 | biostudies-literature | 2016 May

REPOSITORIES: biostudies-literature

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Possible scenarios for occurrence of M ~ 7 interplate earthquakes prior to and following the 2011 Tohoku-Oki earthquake based on numerical simulation.

Nakata Ryoko R   Hori Takane T   Hyodo Mamoru M   Ariyoshi Keisuke K  

Scientific reports 20160510


We show possible scenarios for the occurrence of M ~ 7 interplate earthquakes prior to and following the M ~ 9 earthquake along the Japan Trench, such as the 2011 Tohoku-Oki earthquake. One such M ~ 7 earthquake is so-called the Miyagi-ken-Oki earthquake, for which we conducted numerical simulations of earthquake generation cycles by using realistic three-dimensional (3D) geometry of the subducting Pacific Plate. In a number of scenarios, the time interval between the M ~ 9 earthquake and the su  ...[more]

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