Mineralisation associated with fault, vein and shear zone systems can be related to
processes that operated when those systems were active. Despite the complexity of …

The 2009 L'Aquila sequence activated a normal fault system 50 km long in the Central
Apennines, composed of two main NW-trending faults 12–16 km long: the main high angle …

Injecting fluids in the crust, or their extraction, changes pore pressure and poroelastic
stresses. Both pressure and stress changes can promote seismicity and, hence, the seismic …

In this introduction, we review much of the recent work related to stress transfer, earthquake
triggering, and time‐dependent seismic hazard in order to provide context for the special …

Résumé Between November 2019 and January 2021, a series of seismic events were felt by
the population of the city of Strasbourg, France. The first main event (MLv 3.0) that occurred …

On 6 April (01: 32 UTC) 2009 a MW 6.1 normal faulting earthquake struck the axial area of
the Abruzzo region in central Italy. We study the geometry of fault segments using high …

We present seismological evidence for the existence of an actively slipping low‐angle
normal fault (15° dip) located in the northern Apennines of Italy. During a temporary seismic …

After approximately 2 months of swarm‐like earthquakes in the Mogul neighborhood of west
Reno, NV, seismicity rates and event magnitudes increased over several days culminating …

Magmatic‐hydrothermal ore deposits document the interplay between saline fluid flow and
rock permeability. Numerical simulations of multiphase flow of variably miscible …

The MW 6.13 L'Aquila earthquake ruptured the Paganica fault on 2009/04/06 at 01: 32 UTC,
and started a strong sequence of aftershocks. For the first four days, the region north of the …