Time dependent strain following faulting of a porous medium
Explore this paper's citation graph
- Type
- article
- Published
- 1974-05-10
- Cited by
- 79
- References
- 18
- OpenAlex
- https://openalex.org/W2016141764
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:129079398
Keywords
Aftershock, Geology, Pore water pressure, Biot number, Poromechanics
References
- Theory of crystal dislocations
- DISPLACEMENT FUNCTIONS AND LINEAR TRANSFORMS APPLIED TO DIFFUSION THROUGH POROUS ELASTIC MEDIA
- Time‐dependent friction in rocks
- A COMPARISON OF THE THREE-DIMENSIONAL CONSOLIDATION THEORIES OF BIOT AND TERZAGHI
- Aftershocks Caused by Pore Fluid Flow?
- An exact effective stress law for elastic deformation of rock with fluids
- Consolidation Settlement Under a Rectangular Load Distribution
- PLANE STRAIN AND AXIALLY SYMMETRIC PROBLEMS OF THE CONSOLIDATION OF A SEMI-INFINITE CLAY STRATUM
- Earthquake Prediction: Variation of Seismic Velocities before the San Francisco Earthquake
- General Theory of Three‐Dimensional Consolidation
- The mechanics of stick-slip☆
- Earthquake prediction: a physical basis.
- Time‐dependent friction as a possible mechanism for aftershocks
- Slip in a crystal and rupture in a solid due to shear
- Microfractures, aftershocks, and seismicity
- Dilatancy, pore fluids, and premonitory variations of ts/tp travel times
- On the Time Distribution of Aftershocks Accompanying the Recent Major Earthquakes in and near Japan
Cited by
- On the effects of thermally weakened ductile shear zones on postseismic deformation
- Theory of earthquakes
- Propagating discontinuities in ionized porous media
- Theoretical studies of rupture processes in geological materials
- Physically consistent diffusion in media with memory
- An investigation of deformation and fluid flow at subduction zones using newly developed instrumentation and finite element modeling
- Strength changes due to reservoir-induced pore pressure and stresses and application to Lake Oroville
- Gravity anomaly and density structure of the San Andreas fault zone
- Singularity solution of Lanir’s osmoelasticity: verification of discontinuity simulations in soft tissues
- Fluid mass sources and point forces in linear elastic diffusive solids
- Deformation of spherical cavities and inclusions in fluid-infiltrated elastic materials
- Applications of Elastic Waves to Electronic Devices, Nondestructive Evaluation, and Seismology
- Pore pressure effects in crustal processes
- Postseismic stress and pore pressure readjustment and aftershock distributions
- Coupled deformation-diffusion effects in the mechanics of faulting and failure of geomaterials
- Instability on a weakening fault
- Brecciation processes in fault zones: Inferences from earthquake rupturing
- Seismic waveform attributes before and after the Loma Prieta earthquake: Scattering change near the earthquake and temporal recovery
- Diffusion of fluids in porous media with memory
- Strike-slip fault bridge fluid pumping mechanism: insights from field-based palaeostress analysis and numerical modelling
Related papers
- Convergence of poroelastic finite elements based on Biot displacement formulation
- An assessment of the effective density fluid model for scattering from poroelastic sediments with inclusions
- An assessment of the effective density fluid model for backscattering from rough poroelastic interfaces
- Interface conditions for Biot’s equations of poroelasticity
- Steady‐state harmonic response of a rigid plate bearing on a liquid‐saturated poroelastic halfspace
- On the causes of pressure oscillations in low‐permeable and low‐compressible porous media
- Unsteady Oscillations of a Liquid-Saturated Poroelastic Soil Layer