Tectonic stress in the crust evolves during a seismic cycle, with slow stress accumulation over interseismic periods, episodic stress steps at the time of earthquakes, and …
Magmatic intrusions release extensional strain in the Earth's crust upon availability of magma.
While dynamic earthquake triggering has been reported in several continental settings, offshore observations are rare.
The estimation of space and time-dependent earthquake probabilities, including aftershock sequences, has received increased attention in recent years.
The spatiotemporal clustering of earthquakes is a feature of medium- and short-term seismicity, indicating that earthquakes interact.
Stress transfer between earthquakes is recognized as a fundamental mechanism governing aftershock sequences.
Seismicity closely related to hydrological impacts has been observed in several locations worldwide, particularly in intraplate areas where tectonic stressing rates are small.