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 …

Despite decades of observational, laboratory and theoretical studies, the processes leading
to large earthquake generation remain enigmatic. However, recent observations provide …

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 …

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 …

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 …

The frictional rupture mechanisms of rock discontinuities considering the dynamic load
disturbance still remain unclear. This paper investigates the transitional behaviors of slip …

Temporal changes in seismic velocity during the earthquake cycle have the potential to
illuminate physical processes associated with fault weakening and connections between the …

Recent geodetic observations indicate that a single fault may slip slowly and silently or fast
and seismically in different circumstances. We report laboratory experiments that …

The recognition of slow earthquakes in geodetic and seismological data has transformed the
understanding of how plate motions are accommodated at major plate boundaries. Slow …

Dynamic modeling of sequences of earthquakes and aseismic slip (SEAS) provides a self‐
consistent, physics‐based framework to connect, interpret, and predict diverse geophysical …