1887

Abstract

Summary

The management of induced seismicity during hydraulic stimulations and other injection or extraction operations benefits greatly from any information on geohazards or the state of stress in the subsurface. The ability for pore-pressure and poro-elastic stress perturbations to propagate beyond a modest buffer around the reservoir has underscored the need for such knowledge over a footprint wider than the pad. Often, the seismicity itself allows for such knowledge to be brought better into focus. Locating events with precision will illuminate fault geometries that are often unobserved though other means. By recording with a sufficiently dense network, enough lower magnitude events will be observed to maximize the opportunities to image these faults. For larger events recorded across a sufficiently dense network, the first motions of the P and S waves can constrain the moment tensors, allowing for possible fault geometries to be explored, the faulting regime to be understood with greater nuance, and the stress and strains in and around the reservoir to be understood.

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/content/papers/10.3997/2214-4609.202131030
2021-03-01
2024-04-24
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References

  1. Angelier, J.
    1979. Determination of the mean principal directions of stresses for a given fault population.Tectonophysics56, pp T17–T26.
    [Google Scholar]
  2. Gephart, J. W. and Forsyth, D. W.
    1984. An improved method for determining the regional stress tensor using earthquake focal mechanism data: application to the San Fernando earthquake sequence.J. Geophys. Res.89, pp 9305–9320.
    [Google Scholar]
  3. Michael, A. J.
    1984. Determination of stress from slip data: faults and folds.J. Geophys. Res.89, pp 11517–11526
    [Google Scholar]
  4. Simpson, R. W.
    1997. Quantifying Anderson’s fault types.J. Geophys. Res, 102, pp 17909–17919. https://doi.org/10.1029/97JB01274
    [Google Scholar]
  5. Shen, L., Schmitt, D. R., and Haug, K.
    , 2019. Quantitative constraints to the complete state of stress from the combined borehole and focal mechanism inversions: Fox Creek, Alberta.Tectonophysics, 764, https://doi.org/10.1016/j.tecto.2019.04.023
    [Google Scholar]
  6. Vavryčuk, V.
    2014. Iterative joint inversion for stress and fault orientations from focal mechanisms.Geophys. J. Int.199, pp 69–77, https://dx.doi.org/10.1093/gji/ggu224
    [Google Scholar]
  7. Waldhauser, F. and Ellsworth, W. L.
    2000. A double-difference earthquake location algorithm: method and application to the Northern Hayward Fault, California.Bull. Seism. Soc. Am.90, pp 1351–1368.
    [Google Scholar]
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