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 …

We develop new empirical scaling laws for rupture width W⁠, rupture length L⁠, rupture
area A⁠, and average slip D⁠, based on a large database of rupture models. The database …

Subduction zone plate boundary megathrust faults accommodate relative plate motions with
spatially varying sliding behavior. The 2004 Sumatra‐Andaman (Mw 9.2), 2010 Chile (Mw …

We describe and present a new model of global subduction zone geometries, called Slab1.
0. An extension of previous efforts to constrain the two‐dimensional non‐planar geometry of …

This contribution to the Electronic Seismologist presents the online SRCMOD database of
finite-fault rupture models for past earthquakes, accessible at http://equake‑rc. info/srcmod …

Many studies have modeled the Tohoku tsunami of March 11, 2011 as being due entirely to
slip on an earthquake fault, but the following discrepancies suggest that further research is …

The shallower portions of subduction zone megathrust faults host Earth's most hazardous
tsunamigenic earthquakes, yet understanding how and when they slip remains elusive …

Here, I present a database of> 160 finite fault models for all earthquakes of M 7.5 and above
since 1990, created using a consistent modeling approach. The use of a common approach …

Focal mechanism and slip history of the 2011 M w 9.1 off the Pacific coast of Tohoku, Japan
earthquake were derived rapidly from teleseismic body and surface waves. Multiple double …