Abstract The Geodesy Advancing Geosciences and EarthScope (GAGE) Facility Global
Positioning System (GPS) Data Analysis Centers produce position time series, velocities …

Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

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 …

Abstract On February 6, 2023, an Mw7. 8 earthquake hit the East Anatolian Fault (EAF) and
Narlı Fault (NF), followed by an Mw7. 5 event on the Sürgü Fault. We combine multiple …

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 …

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 …

On 11 March 2011, the devastating M9. 0 Tohoku Earthquake occurred on the interface of
the subducting Pacific plate, and was followed by a huge tsunami that killed about 20,000 …

In the first edition, we paid attention not only to tsunami waves, but to related phenomena,
namely, seaquakes, as well, which to a significant extent reflected the interests of the …

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 …