Our models and understanding of the dynamics of earthquake rupture are based largely on
estimates of earthquake source parameters, such as stress drop and radiated seismic …

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 …

The 2024 moment magnitude 7.5 Noto Peninsula (Japan) earthquake caused devastation to
communities and was generated by a complex rupture process. Using space geodetic and …

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 …

We calculate stress drops for 176 earthquakes (M2. 6-M6. 6) from four sequences of
earthquakes in New Zealand. Two sequences are within the subducting Pacific plate …

Scaling of dynamic rupture processes from small to large earthquakes is critical to seismic
hazard assessment. Large subduction earthquakes are typically remote, and we mostly rely …

During the 2011 magnitude 9 Tohoku-oki earthquake, very large slip occurred on the
shallowest part of the subduction megathrust. Quantitative information on the shallow slip is …

Numerous observations pertaining to the magnitude 9.0 2011 Tohoku-oki earthquake
(offshore Japan) have led to new understanding of subduction zone earthquakes. By …

Aftershocks region have been extensively reported to expand logarithmically with time. The
associated migration velocity is typically of the order of several km/decade but can be much …

The unprecedented geophysical and hydrographic data sets from the 2011 Tohoku
earthquake and tsunami have facilitated numerous modeling and inversion analyses for a …