Reservoir-triggered Seismicity: Difference between revisions
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(Created page with "__NOTOC__ Category: Seismic ---- If the proposed reservoir is substantial in volume or active faults cross near the reservoir area, then potential for reservoir-triggered seismicity (RTS) should be evaluated. RTS is the idea that the added weight of the reservoir or pore pressure distribution increases the frequency of earthquakes in areas of high seismic activity OR may cause earthquakes in areas thought to be seismically inactive. RTS has been observed in dams over...") |
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If the proposed reservoir is substantial in volume or active faults cross near the reservoir area, then potential for reservoir-triggered [[seismicity]] (RTS) should be evaluated. RTS is the idea that the added weight of the reservoir or pore pressure distribution increases the frequency of earthquakes in areas of high [[seismic]] activity | If the proposed reservoir is substantial in volume or active faults cross near the reservoir area, then potential for reservoir-triggered [[seismicity]] (RTS) should be evaluated. RTS is the idea that the added weight of the reservoir or pore pressure distribution increases the frequency of earthquakes in areas of high [[seismic]] activity or may cause earthquakes in areas thought to be seismically inactive. RTS has been observed in dams over 100 meters high. | ||
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Revision as of 20:55, 20 December 2022
If the proposed reservoir is substantial in volume or active faults cross near the reservoir area, then potential for reservoir-triggered seismicity (RTS) should be evaluated. RTS is the idea that the added weight of the reservoir or pore pressure distribution increases the frequency of earthquakes in areas of high seismic activity or may cause earthquakes in areas thought to be seismically inactive. RTS has been observed in dams over 100 meters high.
Citations:
Revision ID: 6119
Revision Date: 12/20/2022