Abstract The 2011 March 11 Tohoku-oki great (Mw 9.1) earthquake ruptured the plate
boundary megathrust fault offshore of northern Honshu with estimates of shallow slip of 50 m …

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 …

Repeating earthquakes (repeaters) that rupture the same fault area (patch) are interpreted to
be caused by repeated accumulation and release of stress on the seismic patch in a …

The 2011 Tohoku-Oki earthquake ruptured a large source region, which included areas with
a range of past M 7 to M 8 earthquakes, varying stress accumulation, and different structural …

We examined the effects of pore fluid pressure on seismicity changes following the 2011 off
the Pacific coast of Tohoku (Tohoku-oki) earthquake through the analysis of aftershocks …

Slow earthquakes are mainly distributed in the vicinity of seismogenic zones of megathrust
earthquakes and relationships between both types of earthquakes are expected. We …

We propose a new energy‐based method to construct rupture scenarios for anticipated
megathrust earthquakes by using an interseismic slip‐deficit model. Our method bridges the …

In the literature, the inverted coseismic slip models from seismological and geodetic data for
the 2011 Tohoku-Oki earthquake portray significant discrepancies, in particular regarding …

We investigated spatiotemporal change in the interplate seismic activity following the 2011
Tohoku‐oki earthquake (M9. 0) in the region where interseismic interplate coupling was …

Quantifying the stress distribution or finding mechanically coupled areas on the plate
interface is fundamentally important for conjecturing megathrust earthquakes that may occur …