Earthquake precursory processes have been central to scientific inquiry for nearly a century.
Recent advancements in earthquake monitoring, geodesy, and data analysis including …

Earthquakes are rupture-like processes that propagate along tectonic faults and cause
seismic waves. The propagation speed and final area of the rupture, which determine an …

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 …

Understanding the physical mechanisms which link fluid injection with triggered
earthquakes is critical in minimizing hazard in subsurface fluid‐injection operations …

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

Earthquakes occur mainly on active faults. Fault slip is closely related to seismicity and is
thus widely discussed in Geosciences, Seismology, and Engineering. Slip experiment is a …

Dynamic failure in the laboratory is commonly preceded by many foreshocks which
accompany premonitory aseismic slip. Aseismic slip is also thought to govern earthquake …

Tectonic faults fail in a spectrum of modes, ranging from earthquakes to slow slip events.
The physics of fast earthquakes are well described by stick–slip friction and elastodynamic …

Earthquake forecasting and prediction have long and in some cases sordid histories but
recent work has rekindled interest based on advances in early warning, hazard assessment …

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 …