Since the catastrophic Sumatra–Andaman tsunami took place in 2004, 16 other tsunamis
have resulted in significant damage and 14 in casualties. We review the fundamental …

For years, many studies of subduction zones and on-land fold-and-thrust belts have
assumed that the frontal portions of accretionary prisms are too weak to rupture …

Seismological data provide evidence of a depth-dependent rupture behaviour of
earthquakes occurring at the megathrust fault of subduction zones, also known as …

We use campaign and continuous GPS measurements at 49 sites between 1996 and 2010
to describe the long‐term active deformation in and near the Nicoya Peninsula …

We develop an updated radiated seismic energy E catalog of global earthquakes with
seismic moment M0≥ 1019 Nm (MW≥ 6.7) from 1997 through mid‐2010, recording 342 …

Abstract Probabilistic Tsunami Hazard Assessment (PTHA) often proceeds by constructing a
suite of hypothetical earthquake scenarios, and modelling their tsunamis and occurrence …

This study tests three models for generating stochastic earthquake-tsunami scenarios on
subduction zones by comparison with deep ocean observations from 18 tsunamis during the …

A new dense and widely distributed tsunami observation network installed off northeast
Japan detected millimeter‐scale tsunamis from an Mw 6.0 shallow interplate earthquake on …

The first 25 h of the aftershock sequence following the 11 March 2011 Mw 9.0 Tohoku,
Japan earthquake is investigated using a backprojection method. In total, 600 aftershocks …

On 4 January 1907, an earthquake occurred off the west coast of Sumatra, Indonesia, with
an instrumental surface-wave magnitude (MS) in the range of 7.5–8.0 at periods of~ 40 s …