Induced Seismicity Potential in Energy Technologies (2013)

Chapter: Appendix C: Observations of Induced Seismicity

Previous Chapter: Appendix B: Meeting Agendas
Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.

APPENDIX C

Observations of Induced Seismicity

Site/City/StateCountryMax MagnitudeTechnology Type (causing induced seismicity)Reference
AkmaarNetherlands3.5Oil and gas extractionGiardini (2011)
AkosomboGhana5.3Surface water reservoirGuha (2000)
Apollo Hendrick Field, TexasUSA2Secondary recoveryDoser et al. (1992)
Ashtabula, OhioUSA3.6Wastewater injectionArmbruster et al. (1987)
AssenNetherlands2.8Oil and gas extractionGrasso (1992)
AswanEgypt5.6Surface water reservoirGuha (2000)
Attica, New YorkUSA5.2OtherNicholson and Wesson (1992)
Bad UrachGermany1.8GeothermalEvans et al. (2012)
Bajina BastaYugoslavia4.8Surface water reservoirGuha (2000)
Barsa-Gelmes-Wishka OilfieldTurkmenistan6Secondary recoveryKouznetsov et al. (1994)
BaselSwitzerland3.4GeothermalGiardini (2011)
BelchalowPoland4.6OtherGiardini (2011)
BenmoreNew Zealand5Surface water reservoirGuha (2000)
Bergermeer FieldNetherlands3.5Oil and gas extractionvan Eck et al. (2006)
BerlinEl Salvador4.4GeothermalBommer et al. (2006)
BhatsaIndia4.8Surface water reservoirGuha (2000)
BlackpoolUK2.3Hydraulic fracturingde Pater and Baisch (2011)
Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
Site/City/StateCountryMax MagnitudeTechnology Type (causing induced seismicity)Reference
Wilmington Field, CaliforniaUSA3.3Oil and gas extractionKovach (1974)

NOTE: “Other” refers to, e.g., coal and solution mining.

1 Nicholson and Wesson (1990, 1992) were not able to confirm that the cause of the earthquake was oil and gas extraction; waterflooding and waste disposal were also active in the area at the time.

2 Nicholson and Wesson (1990, 1992) were not able to confirm the accuracy of the maximum magnitude of this event, which occurred at the turn of the 20th century (1898-1907).

3 For the Denver earthquakes of 1967-1968, Healy et al. (1968) reported magnitudes up to M 5.3 on an unspecified scale that were derived from local instruments.

4 Nicholson and Wesson (1992) were not able to confirm conclusively that the earthquake was caused by oil and gas extraction.

5 Nicholson and Wesson (1992) were not able to confirm conclusively that the earthquake was caused by oil extraction or the magnitudes of the events that occurred in the 1920s. Note that this location is not plotted in the figures (maps) in Chapter 1.

6 Guha (2000) describes the earthquake using Modified Mercalli Intensity (V), but does not indicate moment magnitude.

7 Nicholson and Wesson (1990, 1992) were not able to confirm conclusively that the event(s) were due to waterflooding for secondary recovery.

8 Nicholson and Wesson (1990) were not able to confirm conclusively that the event(s) were due to oil and gas extraction activities.

9 Nicholson and Wesson (1990) were not able to confirm the maximum magnitude of the events at this site.

10 Nicholson and Wesson (1990, 1992) were not able to confirm conclusively that the event(s) were due to oil extraction.

11 Nicholson and Wesson (1992) were not able to confirm the maximum magnitude of the events at this site.

12 Zoback and Zinke (2002) did not provide a maximum magnitude, although the events recorded and analyzed are described as “microseismic” events.

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Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.

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Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
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Suggested Citation: "Appendix C: Observations of Induced Seismicity." National Research Council. 2013. Induced Seismicity Potential in Energy Technologies. Washington, DC: The National Academies Press. doi: 10.17226/13355.
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Next Chapter: Appendix D: Letters between Senator Bingaman and Secretary Chu
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