Seismic velocity changes associated with aseismic deformations of a fault stimulated by fluid injection
Journal Article
·
· Geophysical Research Letters
- Univ. of Côte d'Azur, Géoazur (France). Côte d'Azur Observatory (OCA)
- Aix-Marseille Univ., Marseille (France). European Center of Research and Teaching of Environmental Geosciences (CEREGE)
- Univ. of Côte d'Azur, Géoazur (France). Côte d'Azur Observatory (OCA); Institut Universitaire de France, Paris (France)
- Total, Exploration and Production, Research and Development, Pau (France)
Fluid pressure plays an important role in the stability of tectonic faults. However, the in situ mechanical response of faults to fluid pressure variations is still poorly known. To address this question, we performed here a fluid injection experiment in a fault zone in shales while monitoring fault movements at the injection source and seismic velocity variations from a near-distance (<10 m) monitoring network. We measured and located the P and S wave velocity perturbations in and around the fault using repetitive active sources. We observed that seismic velocity perturbations dramatically increase above 1.5 MPa of injection pressure. This is consistent with an increase of fluid flow associated with an aseismic dilatant shearing of the fault as shown by numerical modeling. We find that seismic velocity changes are sensitive to both fault opening by fluid invasion and effective stress variations and can be an efficient measurement for monitoring fluid-driven aseismic deformations of faults.
- Research Organization:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Organization:
- Total S.A. (France)
- OSTI ID:
- 1480737
- Journal Information:
- Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 18 Vol. 43; ISSN 0094-8276
- Publisher:
- American Geophysical UnionCopyright Statement
- Country of Publication:
- United States
- Language:
- English
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