Seismic events attributable to human activities are called induced seismic events, although a distinction should be made between: i) induced seismicity where the stress change caused by the geothermal operation is comparable with the ambient stress acting on a fault, and ii) triggered seismicity where the stress variation induced by geothermal activity is only a small fraction of the natural tectonic stress field (McGarr, 2002). Geothermal development tends to modify the characteristics of a reservoir by withdrawing and injecting hot and/or cold fluid into the underground and has a limited potential to cause felt seismic events. Production and injection rates and pressures, fluid volumes, and injection duration are factors that affect the likelihood and magnitude of induced seismic events.
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