摘要：The 2008 Iwate-Miyagi Nairiku Earthquake ( M j 7.2) occurred on June 14, 2008, at the eastern flank of the Ou backbone range, in the central part of northern Honshu, Japan.In the northern part of the focal area, seismic reflection/refraction experiments conducted in 2006 and 2007 revealed a series of west-dipping faults.To investigate the relation between these faults and aftershocks, we conducted a high-density seismic array observation across the northern focal area.The arrival times of earthquakes were used in a joint inversion for earthquake locations and velocity structure.The V p structure shows tilted blocks and the block boundaries coincide with the revealed west-dipping faults.These faults were interpreted to have formed during the Miocene extension.The aftershock distribution shows a concentration on a plane dipping westward approximately 40° beneath the eastern margin of the Ou backbone range.The zone of aftershock concentration can be correlated to the known range-bounding fault inferred from seismic profiling and does not coincide with the known active reverse fault (Dedana fault).These results indicate the significance of the potential source fault located along the boundary of the Ou backbone range. Key words The 2008 Iwate-Miyagi Nairiku Earthquake high-density seismic array observation seismic tomography aftershock distribution fault reactivation.
