In the most destructive and catastrophic landslide events, rocks, soil and fluids can travel at
speeds approaching several tens of metres per second. However, many landslides …

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

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 …

Slow earthquakes represent an important conundrum in earthquake physics. While regular
earthquakes are catastrophic events with rupture velocities governed by elastic wave speed …

Faults in Earth's crust accommodate slow relative motion between tectonic plates through
either similarly slow slip or fast, seismic-wave-producing rupture events perceived as …

Since their discovery two decades ago,, slow slip events have been shown to play an
important role in accommodating strain in subduction zones. However, the physical …

We performed laboratory friction experiments on shale samples from three hydrocarbon
reservoirs to assess compositional controls on fault slip behavior accompanying hydraulic …

Nonvolcanic tremor is observed in close association with geodetically observed slow-slip
events in subduction zones. Accumulating evidence points to these events as members of a …

Understanding the physical mechanisms that underpin the link between fluid injection and
seismicity is essential in efforts to mitigate the seismic risk associated with subsurface …

A growing body of observations worldwide has documented fault slip transients that radiate
little or no seismic energy. The mechanisms that govern these slow slip events (SSEs) and …