Spatiotemporal Evolution of Pore Pressure Changes and Coulomb Failure Stress in a Poroelastic Medium for Different Faulting Regimes
Abstract Spatial distribution of aftershocks has been explained by the co‐seismic static Coulomb Failure Stress changes (ΔCFS) to some extent. In practice, the earth's crust is porous medium saturated with fluid filling pores, cavities, cracks, and faults. The pore fluid flow plays an important...
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| Auteurs principaux: | , , , , , |
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| Format: | article |
| Langue: | EN |
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American Geophysical Union (AGU)
2021
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| Accès en ligne: | https://doaj.org/article/d00b210a36514ef9badd24fc1e846c82 |
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