The 2016– 2017 Central Apennines earthquake sequence is a recent example of how damages from subsequent aftershocks can exceed those caused by the initial mainshock.
The static coulomb stress hypothesis is a widely known physical mechanism for earthquake triggering and thus a prime candidate for physics-based operational earthquake forecasting …
Magmatic intrusions release extensional strain in the Earth's crust upon availability of magma.
The estimation of space and time-dependent earthquake probabilities, including aftershock sequences, has received increased attention in recent years.
Seismicity closely related to hydrological impacts has been observed in several locations worldwide, particularly in intraplate areas where tectonic stressing rates are small.