pure and applied geophysics

, Volume 139, Issue 3–4, pp 561–578 | Cite as

Triggered earthquakes and deep well activities

  • Craig Nicholson
  • Robert L. Wesson


Earthquakes can be triggered by any significant perturbation of the hydrologic regime. In areas where potentially active faults are already close to failure, the increased pore pressure resulting from fluid injection, or, alternatively, the massive extraction of fluid or gas, can induce sufficient stress and/or strain changes that, with time, can lead to sudden catastrophic failure in a major earthquake. Injection-induced earthquakes typically result from the reduction in frictional strength along preexisting, nearby faults caused by the increased formation fluid pressure. Earthquakes associated with production appear to respond to more complex mechanisms of subsidence, crustal unloading, and poroelastic changes in response to applied strains induced by the massive withdrawal of subsurface material. As each of these different types of triggered events can occur up to several years after well activities have begun (or even several years after all well activities have stopped), this suggests that the actual triggering process may be a very complex combination of effects, particularly if both fluid extraction and injection have taken place locally. To date, more than thirty cases of earthquakes triggered by well activities can be documented throughout the United States and Canada. Based on these case histories, it is evident that, owing to preexisting stress conditions in the upper crust, certain areas tend to have higher probabilities of exhibiting such induced seismicity.

Key words

Induced seismicity triggered earthquakes fluid injection fluid extraction 


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  1. Allen, D. R., andMayuga, M. N. (1970),The mechanics of compaction and rebound, Wilmington oil field, Long Beach, California, U.S.A. In Land Subsidence (International Association of the Science of Hydrology, UNESCO Publ.89, 2) pp. 410–423.Google Scholar
  2. Armbruster, J. G., Seeber, L., andEvans, K. (1987),The July 1987 Ashtabula Earthquake (m b 3.6) Sequence in Northeastern Ohio and a Deep Fluid Injection Well (abstract), Seismol. Res. Lett.58, 91.Google Scholar
  3. Caloi, P., DePanfilis, M., DeFilippo, D., Marcelli, L., andSpadea, M. C. (1956),Terrimoti della Val Padana del 15–16 Maggio 1951, Ann Geophys.9, 63–105.Google Scholar
  4. Cox, R. T. (1991),Possible Triggering of Earthquakes by Underground Waste Disposal in the El Dorado, Arkansas Area, Seismol. Res. Lett.62, 113–122.Google Scholar
  5. Davis, S. D. (1985),Investigations of Natural and Induced Seismicity in the Texas Panhandle, M. S. Thesis, University of Texas, Austin, Texas, 230 pp.Google Scholar
  6. Davis, S. D., andPennington, W. D. (1989),Induced Seismic Deformation in the Cogdell Oil Field of West Texas, Bull. Seismol. Soc. Am.79, 1477–1495.Google Scholar
  7. Doser, D. I., Baker, M. R., andMason, D. B. (1991),Seismicity in the War-Wink Gas Field, Delaware Basin, West Texas, and its Relationship to Petroleum, Bull. Seismol. Soc. Am.81, 971–986.Google Scholar
  8. Evans, D. M. (1966),The Denver Area Earthquakes and the Rocky Mountain Arsenal Disposal Well, Mountain Geologist3, 23–36.Google Scholar
  9. Evans, K. F. (1988),Assessing Regional Potential for Induced Seismicity from Crustal Stress Measurements: An Example from Northern Ohio, NCEER Technical Rep., 30 pp.Google Scholar
  10. Fletcher, J. B., andSykes, L. R. (1977),Earthquakes Related to Hydraulic Mining and Natural Seismic Activity in Western New York State, J. Geophys. Res.82, 3767–3780.Google Scholar
  11. Hamilton, D. H., andMeehan, R. L. (1971),Ground Rupture in the Baldwin Hills, Science172, 333–344.Google Scholar
  12. Harding, S. T. (1981),Induced Seismicity in the Cogdell Canyon Reef Oil Field, U.S. Geol. Surv. Open-file Report81-167, 452–455.Google Scholar
  13. Healy, J. H., Rubey, W. W., Griggs, D. T., andRaleigh, C. B. (1968),The Denver Earthquakes, Science161, 1301–1310.Google Scholar
  14. Hsieh, P. A., andBredehoeft, J. D. (1981),A Reservoir Analysis of the Denver Earthquakes: A Case of Induced Seismicity, J. Geophys. Res.86, 903–920.Google Scholar
  15. Kovach, R. L. (1974),Source Mechanisms for Wilmington Oil Field, California, Subsidence Earthquakes, Bull. Seismol. Soc. Am.64, 699–711.Google Scholar
  16. McGarr, A. (1991),On a Possible Connection between three Major Earthquakes in California and Oil Production, Bull Seismol. Soc. Am.81, 948–970.Google Scholar
  17. Mereu, R. F., Brunet, J., Morrissey, K., Price, B., andYapp, A. (1986),A Study of the Microearthquakes of the Gobles Oilfield Area of Southwestern Ontario, Bull. Seismol. Soc. Am.76, 1215–1223.Google Scholar
  18. Milne, W. G., andBerry, M. J. (1976),Induced Seismicity in Canada, Eng. Geol.10, 219–226.Google Scholar
  19. Nicholson, C., Roeloffs, E., andWesson, R. L. (1988),The Northeastern Ohio Earthquake of January 31, 1986—Was it Induced?, Bull Seismol. Soc. Am.78, 188–217.Google Scholar
  20. Nicholson, C., andWesson, R. L. (1990),Earthquake Hazard Associated with Deep Well Injection, U.S. Geol. Surv. Bull. 1951, 74 pp.Google Scholar
  21. Pearson, C. (1981),The Relationship between Microseismicity and High Pore Pressures during Hydraulic Stimulation Experiments in Low Permeability Granitic Rocks, J. Geophys. Res.86, 7855–7864.Google Scholar
  22. Pennington, W. D., Davis, S. D., Carlson, S. M., DuPree, J., andEwing, T. E. (1986),The Evolution of Seismic Barriers and Asperities Caused by the Depressuring of Fault Planes in Oil and Gas Fields of South Texas, Bull. Seismol. Soc. Am.76, 939–948.Google Scholar
  23. Pratt, W. E., andJohnson, D. W. (1926),Local Subsidence of the Goose Creek Oil Field, J. Geol.34, 577–590.Google Scholar
  24. Raleigh, C. B., Healy, J. H., andBredehoeft, J. D. (1972),Faulting and crustal stress at Rangely, Colorado. InFlow and Fracture of Rocks (AGU Geophys. Monogr. Series16) pp. 275–284.Google Scholar
  25. Raleigh, C. B., Healy, J. H., andBredehoeft, J. D. (1976),An Experimental in Earthquake Control at Rangely, Colorado, Science191, 1230–1237.Google Scholar
  26. Richter, C. F.,Elementary Seismology (W. H. Freeman and Co., San Francisco and London 1958) 768 pp.Google Scholar
  27. Rothe, G. H., andLui, C.-Y. (1983),Possibility of Induced Seismicity in the Vicinity of the Sleepy Hollow Oil Field. Southwestern Nebraska, Bull. Seismol. Soc. Am.73, 1357–1367.Google Scholar
  28. Segall, P. (1989),Earthquakes Triggered by Fluid Extraction, Geology17, 942–946.Google Scholar
  29. Sibson, R. H. (1992),Implications of Fault-valve Behavior for Rupture Nucleation and Recurrence, Tectonophysics211, 283–293.Google Scholar
  30. Simpson, D. W. (1986),Triggered Earthquakes, Ann. Rev. Earth Planet Sci.14, 21–42.Google Scholar
  31. Simpson, D. W., Kebeasy, R. M., Maamoun, M., Albert, R., andBoulois, F. K. (1982),Induced Seismicity at Aswan Lake, Egypt (abstract), EOS, Trans. Am. Geophys. Union63, 371.Google Scholar
  32. Simpson, D. W., andLeith, W. (1985),The 1976 and 1984 Gazli, U.S.S.R. Earthquakes — Were they Induced?, Bull. Seismol. Soc. Am.75, 1465–1468.Google Scholar
  33. Teng, T. L., Real, C. R., andHenyey, T. L. (1973),Microearthquakes and Water Flooding in Los Angeles, Bull. Seismol. Soc. Am.63, 859–875.Google Scholar
  34. Wetmiller, R. J. (1986),Earthquakes near Rocky Mountain House, Alberta, and their Relationship to Gas Production Facilities, Canadian J. Earth Science23, 172–181.Google Scholar
  35. Yerkes, R. F., andCastle, R. D. (1976),Seismicity and Faulting Attributed to Fluid Extraction, Eng. Geol.10, 151–167.Google Scholar

Copyright information

© Birkhäuser Verlag 1992

Authors and Affiliations

  • Craig Nicholson
    • 1
  • Robert L. Wesson
    • 2
  1. 1.Institute for Crustal StudiesUniversity of CaliforniaSanta BarbaraUSA
  2. 2.U.S. Geological SurveyMS905 National CenterRestonUSA

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