Due to the deep socioeconomic implications, induced seismicity is a timely and increasingly
relevant topic of interest for the general public. Cases of induced seismicity have a global …

The ability of fluid-generated subsurface stress changes to trigger earthquakes has long
been recognized. However, the dramatic rise in the rate of human-induced earthquakes in …

The combination of hybrid perovskite and Cu (In, Ga) Se2 (CIGS) has the potential for
realizing high-efficiency thin-film tandem solar cells because of the complementary tunable …

Wastewater disposal in the central US is likely responsible for an unprecedented surge in
earthquake activity. Much of this activity is thought to be driven by induced pore pressure …

Fluid injection can cause extensive earthquake activity, sometimes at unexpectedly large
distances. Appropriately mitigating associated seismic hazards requires a better …

The basic triggering mechanism underlying induced seismicity traces back to the mid‐1960s
that relied on the process of pore‐fluid pressure diffusion. The last decade has experienced …

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

Anthropogenic fluid injections at depth induce seismicity which is generally organized as
swarms, clustered in time and space, with moderate magnitudes. Earthquake swarms also …

It is well established that fluid injection has the potential to induce earthquakes—from
microseismicity to magnitude 5+ events—by altering state-of-stress conditions in the …

Fluid injections into the deep subsurface can, at times, generate earthquakes, but often, they
only produce aseismic deformations. Here we analyze the influence of fault …