Abstract
This study considers the effects of heat transfer and fluid flow on the thernal, hydrologic, and mechanical response of a fault surface during seismic failure. Numerical modeling techniques are used to account for the coupling of the thermal, fluid-pressure, and stress fields. Results indicate that during an earthquake the failure surface is heated to a tempeature required for the thermal expansion of pore fluids to balance the rate of fluid loss due to flow and the fluid-volume changes due to pore dilatation. Once this condition is established, the pore fluids pressurize and the shear strength decreases rapidly to a value sufficient to maintain the thermal pressurization of pore fluids at near-lithostatic values. If the initial fluid pressure is hydrostatic, the final temperature attained on the failure surface will increase with depth, because a greater pressure increase can occur before a near-lithostatic pressure is reached. The rate at which thermal pressurization proceeds depends primarily on the hydraulic characteristics of the surrounding porous medium, the coefficient of friction on the fault surface, and the slip velocity. If either the permeability exceeds 10−15 m2 or the porous medium compressibility exceeds 10−8 Pa−1, then frictional melting may occur on the fault surface before thermal pressurization becomes significant. If the coefficient of friction is less than 10−1 and if the slip velocity is less than 10−2 msec−1, then it is doubtful that either thermal pressurization or frictional melting on the fault surface could cause a reduction in the dynamic shear strength of a fault during an earthquake event.
Similar content being viewed by others
References
Boit, M. A. (1941),General Theory of Three Dimensional Consolidation, J. Appl. Phys.12, 155–164.
Biot, M. A., andWillis, D. G. (1957),The Elastic Coefficients of the Theory of Consolidation, J. Appl. Mech.24, 594–601.
Byerlee, J. D. (1978),Friction of Rocks, Pure Appl. Geophys.116, 615–626.
Cardwell, R. K., Chinn, D. S., Moore, G. F., andTurcotte, D. L. (1978),Frictional Heating on a Fault of Finite Thickness, Geophys. J. Roy. Astron. Soc.52, 525–530.
Carslaw, H. C., andJaeger, J. C. (1959),Conduction of Heat in Solids, Oxford Univ. Press, New York, 386 pp.
Delaney, P. T. (1982),Rapid Intrusion of Magma Into Wet Rock: Groundwater Flow Due to Pore Pressure Increases, J. Geophys. Res.87 (B9), 7739–7756.
Domenico, P. A., andPalciauskas, V. V. (1979a),Thermal Expansion of Fluids and Fracture Initiation in Compacting Sediments, II, Bull. Geol. Soc. Am.90, 953–979.
Domenico, P. A., andPalciauskas, V. V. (1979b),Thermal Expansion of Fluids and Fracture Initiation in Compacting Sediments, II, Bull. Geol. Soc. Am.90, 953–979.
Holcomb, D. J. (1978),A Quantitative Model of Dilatancy in Dry Rock and its Application to Westerly Granite, J. Geophys. Res.83 (B10), 4941–4950.
Holcomb, D. J. (1981),Memory, Relaxation, and Microfracturing in Dilatant Rock, J. Geophys. Res.86 (B7), 6235–6248.
Jaeger, J. C. (1942),Moving sources of heat and temperature at sliding contacts, J. Proc. R. Soc. N.S.W.76, 203–224.
Jorgensen, D. G. (1981),Relationships Between Basic Soils-Engineering Equations and Basic Ground Water Flow Equations, U.S. Geol. Survey Water-Supply Paper, 2064, 46 pp.
Keenan, J. H., Keyes, F. G., Hill, P. G., andMoore, J. G.,Steam Tables (Wiley, New York 1978), 162 pp.
Kestin, J. (1978),Thermal Conductivity of Water and Steam, Mech Eng.100(8), 1255–1258.
Lachenbruch, A. H. (1980),Frictional Heating, Fluid Pressure, and the Resistance to Fault Motion, J. Geophys. Res.85(B11), 6097–6112.
Lachenbruch, A. H., Sass, J. H., Munroe, R. J., andMoses, T. H., Jr. (1976),Geothermal Setting and Simple Heat Conduction Models for the Long Valley Caldera, J. Geophys. Res.81, 769–784.
Lockner, D. A., andOkubo, P. G. (1983),Measurements of Frictional Heating in Granite, J. Geophys. Res.88(B5), 4313–4320.
Logan, J. M. (1979),Brittle Phenomena, Rev. Geophys. Space Phys.17, 1121–1132.
Mase, C. W. (1985),The Role of Shear-Strain Heating and Pore-Fluid Pressures on the Dynamics of Fault Zone Processes, Ph.D. Thesis, Univ. British Columbia, Vancouver, Canada.
McKenzie, D. P., andBrune, J. N. (1972),Melting of Fault Planes During Large Earthquakes, Geophys. J. Roy. Astron. Soc.29, 65–78.
Morrow, C. A., Shi, L. Q., andByerlee, J. D. (1982),Strain hardening and strength of clay-rich fault gouges, J. Geophys. Res.87, 6771–6780.
Nur, A. (1978),Nonuniform Friction as a Physical Basis for Earthquake Mechanics, Pure Appl. Geophys.116, 964–989.
Nur, A., andBooker, J. R. (1972),Aftershocks Caused by Pore Fluid Flow, Science146, 1003–1010.
Nur, A., andByerlee, J. D. (1971),An Exact Effective Stress Law for Elastic Deformation of Rock with Fluids, J. Geophys. Res.76, 6414–6419.
Palciauskas, V. V., andDomenico, P. A. (1982),Characterization of Thermally Loaded Repository Rocks, Water Resour. Res.18, 281–290.
Raleigh, B., andEverden, J. Case for Low Deviatoric Stress in the Lithosphere. InThe Mechanical Behavior of Crustal Rocks, Geophys. Monogr. Ser., Vol 24 (eds. N. L. Carter, M. Friedman, J. M. Logan, and D. W. Stearns) (Amer. Geophys. Union 1981), pp. 173–186.
Rice, J. R., andRundnicki, J. W. (1979),Earthquake Precursory Effects Due to Pore Fluid Stabilization of a Weakening Fault Zone, J. Geophys. Res.84(B5), 2177–2193.
Rice, J. R., andSimons, D. A. (1976),The Stabilization of Spreading Shear Faults by Coupled Deformation-Diffusion Effects in Fluid-Infiltrated Porous Media, J. Geophys. Res.81, 5322–5334.
Richards P. G. (1976),Dynamic motions near an earthquake fault: a three dimensional solution, Seism. Soc. Am. Bull.66, 1–32.
Rudnicki, J. W. (1979),The Stabilization of Slip on a Narrow Weakening Fault Zone by Coupled Deformation-Pore Fluid Diffusion, Bull. Seis. Soc. Am.69, 1011–1026.
Sass, J. H., Lachenbruch, A. H., andMunroe, R. J. (1971),Thermal Conductivity of Rocks from Measurements on Fragments and its Application to Heat-Flow Determinations. J. Geophys. Res.76, 3391–3401.
Scholz, C. H., Sykes, L. R., andAggrawal, Y. P. (1973),Earthquake Prediction: A Physical Basis, Science181, 803–810.
Sibson, R. H. (1973),Interactions Between Temperature and Pore-Fluid Pressure During Earthquake Faulting and a Mechanism for Partial or Total Stress Relie, Nature Phys. Sci.243, 66–68.
Sibson, R. H. (1977),Kinetic Shear Resistance, Fluid Pressure and Radiation Efficiency During Seismic Faulting, Pure Appl. Geophys.115, 387–400.
Sibson, R. H. (1980),Power Dissipation and Stress Levels on Faults in the Upper Crust, J. Geophys. Res.85(B11), 6239–6247.
Teufel, L. W., andLogan, J. M. (1979),Effect of Displacement Rate on the Real Area of Contact and Temperatures Generated During Frictional Sliding of Tennessee Sandstone, Pure Appl. Geophys.116, 840–865.
Watson, J. T. R., Basu, R. S., andSengers, J. V. (1980),An Improved Representative Equation for the Dynamic Viscosity of Water Substance, J. Phys. Chem. Ref. Data9(4), 1255–1279.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Mase, C.W., Smith, L. Pore-fluid pressures and frictional heating on a fault surface. PAGEOPH 122, 583–607 (1984). https://doi.org/10.1007/BF00874618
Received:
Revised:
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF00874618