Slow earthquakes are characterized by a wide spectrum of fault slip behaviors and seismic
radiation patterns that differ from those of traditional earthquakes. However, slow …

In a context of global change and increasing anthropic pressure on the environment,
monitoring the Earth system and its evolution has become one of the key missions of …

Modern geodetic and seismologic observations describe the behavior of fault slip over a
vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from …

Predicting failure in solids has broad applications including earthquake prediction which
remains an unattainable goal. However, recent machine learning work shows that laboratory …

Most destructive tsunamis are caused by seismic slip on the shallow part of offshore
megathrusts. The likelihood of this behaviour is partly determined by the interseismic slip …

The discovery of slow earthquakes has revolutionized the field of earthquake seismology.
Defining the locations of these events and the conditions that favor their occurrence provides …

Continuously operating global positioning system sites in the North Island of New Zealand
have revealed a diverse range of slow motion earthquakes on the Hikurangi subduction …

Slow slip events are part of a spectrum of aseismic processes that relieve tectonic stress on
faults. Their spatial distribution in subduction zones has been linked to perturbations in fluid …

Slow slip events (SSEs) accommodate a significant proportion of tectonic plate motion at
subduction zones, yet little is known about the faults that actually host them. The shallow …

Subduction of rough seafloor and seamounts is thought to impact a broad range of
geodynamic processes, including megathrust slip behaviour, forearc fluid flow and long-term …