Earthquakes can change the stress field in the Earth's lithosphere as they relieve and
redistribute stress. Earthquake‐induced stress changes have been observed as temporal …

Abstract The 2011 Mw 9.0 Tohoku‐oki earthquake is one of the world's best‐recorded
ruptures. In the aftermath of this devastating event, it is important to learn from the complete …

The spatiotemporal distributions of hypocenters and temporal change in seismicity patterns
were investigated in details for events in the Yamagata‐Fukushima border earthquake …

After the occurrence of the 2011 magnitude 9 Tohoku earthquake, seismicity in the
overriding plate changed. This chapter considers some possible evidence of the influence of …

Rupture‐zone averaged static stress drop in the 2011 M= 9 Tohoku‐Oki earthquake was
less than 5 MPa, but it caused a stress reversal in most of the offshore forearc, although the …

We present a systematic study of seismic velocity changes associated with a megathrust and
five strong crustal earthquakes in Japan. We perform both cross-correlation and single …

We introduce the single-station cross-correlation (SC) technique of processing ambient
seismic noise and compare its results with the established cross-correlation (CC) and …

Inland Tohoku has been recognized as under the WNW-ESE compressional stress state
before the 2011 M9 Tohoku-Oki earthquake. Earthquakes that occurred there were …

Numerous normal‐faulting aftershocks in subduction forearcs commonly follow large
megathrust earthquakes. Postseismic normal faulting has been explained by stress changes …

Increases in seismicity have been widely observed at varying distances from the source
area following large earthquakes. The increased number of earthquakes are usually called …