Our models and understanding of the dynamics of earthquake rupture are based largely on
estimates of earthquake source parameters, such as stress drop and radiated seismic …

Earthquake swarms may be driven by fluids, through hydraulic injections or natural fluid
circulation, but also by slow and aseismic slip transients. Understanding the driving factors …

Seismic swarms, in natural contexts or induced by anthropogenic fluid injections, commonly
show migrations of earthquake hypocenters. Classically, such migrations are interpreted as …

Fluid‐induced earthquake sequences generally appear as expanding swarms activating a
particular fault. The recent analysis of a swarm in the Corinth rift has revealed a dual …

Identification of repeating earthquakes (repeaters) usually depends on waveform similarity
expressed as the corresponding cross‐correlation coefficient (CC) above a prescribed …

How induced seismicity in deep geothermal project (enhanced geothermal systems, EGS) is
controlled by fluid injection is of central importance for monitoring the related seismic risk …

Repeating earthquakes (repeaters) are events that recurrently rupture the same fault patch
with nearly identical magnitudes. Although repeaters have been widely studied and utilized …

Injection‐induced earthquakes associated with wastewater disposal (WD) in the Western
Canadian Sedimentary Basin are much fewer than those linked to hydraulic fracturing …

The evolution of fluid injection‐induced seismicity, generally characterized through the
number of events or their seismic moment, depends on, among other factors, the injected …

The successful exploitation of geothermal reservoirs relies upon the understanding of fluid
circulation in the subsurface. However, large-scale fluid flow modelling often assumes that …