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 …

Induced seismicity associated with fluid injection into underground formations jeopardizes
the sustainable utilization of the subsurface. Understanding the fault behavior is the key to …

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 …

Faults can slip seismically or aseismically depending on their hydromechanical properties,
which can be measured in the laboratory. Here, we demonstrate that fault slip induced by …

Understanding the response of faults to the injection of high-pressure fluids is important for
several subsurface applications, for example, geologic carbon sequestration or energy …

The addition of water on or below the earth's surface generates changes in stress that can
trigger both stable and unstable sliding of landslides and faults. While these sliding …

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 …

Understanding the physical mechanisms governing fluid‐induced fault slip is important for
improved mitigation of seismic risks associated with large‐scale fluid injection. We …

Modern geophysics highlights that the slip behaviour response of faults is variable in space
and time and can result in slow or fast ruptures. However, the origin of this variation of the …

We studied the influence of stress state and fluid injection rate on the reactivation of faults.
We conducted experiments on a saw cut Westerly granite sample under triaxial stress …