Research news on induced seismicity

Induced seismicity refers to earthquakes and seismic events that are directly or indirectly triggered by human activities that alter the state of stress or pore-fluid pressure in the Earth's crust. Key drivers include fluid injection or withdrawal (e.g., wastewater disposal, geothermal operations, hydrocarbon production), reservoir impoundment, mining, and underground construction. These activities modify effective normal stress on faults, potentially bringing pre-stressed fault segments to failure according to Coulomb failure criteria. Research focuses on characterizing fault activation thresholds, spatiotemporal patterns of seismicity, scaling relationships with operational parameters, and developing probabilistic hazard models and operational protocols (“traffic light” systems) to manage and mitigate seismic risk.

Seismic activity in California varies with the seasons

Earthquakes occur when the tectonic plates of the Earth's crust shift, jolting past each other in a release of built-up tension. However, other natural forces can also influence seismic activity: Hydrological dynamics, like ...

Fracking in Argentina 'linked to hundreds of tremors'

The extraction of gas and oil by fracking—large-scale fracturing of underground rocks by injecting water, sand and additives—is generating growing concern in Argentine Patagonia. Neuquén province—home to the country's largest ...

Cascadia megathrust earthquake could trigger San Andreas fault

When the tectonic subduction zone beneath the Pacific Northwest moves, it does so in dramatic fashion. Not only is ground shaking from a magnitude 9+ earthquake incredibly destructive, the event triggers tsunamis and landslides ...

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