Faulkner D R, Rutter E H. 2000. Comparisons of water and argon permeability in natural clay-bearing fault gouge under high pressure at 20°C. J Geophys Res, 105: 16415-16426
[2]
Faulkner D R, Rutter E H. 2003. The effect of temperature, the nature of the pore fluid, and subyield differential stress on the permeability of phyllosilicate-rich fault gouge. J Geophys Res, 108(B5): 2227
[3]
Fischer G J, Paterson M S. 1992. Measurements of Permeability and Storage Capacity in Rocks during Deformation at High Temperature and Pressure. In: Evans B, Wong T F, eds. Fault Mechanics and Transport Properties of Rocks. New York: Academic Press. 213-52
[4]
Freeman D L, Bush D C. 1983. Low-permeability laboratory measurements by nonsteady-state and conventional methods. Soc Petrol Eng J, 23: 928-936
[5]
Heid J G, McMahon J J, Nielson R F. 1950. Study of the permeability of rocks to homogeneous fluids. Am Pet Inst Drill Prod Pract. 230-244
[6]
Jones F O, Owens W W. 1980. A laboratory study of low-permeability gas sands. J Pet Technol, 32: 1631-1640
[7]
Jones J R, Frank O. 1964. Influence of chemical composition of water on clay blocking of permeability. J Pet Technol, 16: 441-446
[8]
Jones, Stanley C. 1972. Rapid accurate unsteady-state Klinkenberg permeameter. Spe J, 12: 383-397
[9]
Kia S F, Fogler H, Reed M G, et al. 1987. Effect of salt composition on clay release in Berea sandstones. SPE Prod Eng, 2: 277-283
[10]
Klinkenberg L J. 1941. The permeability of porous media to liquids and gases. Am Pet Inst Drill Prod Pract. 200-213
[11]
Kranz R L, Saltzman J S, Blacic J D. 1990. Hydraulic diffusivity measurements on laboratory samples using an oscillating pore pressure method. Int J Rock Mech Min Sci Geomech Abstr, 27: 345-52
[12]
Kwon O, Herbert B, Kronenberg A. 2004. Permeability of illite-bearing shale: 2. Influence of fluid chemistry on flow and functionally connected pores. J Geophys Res, 109: B10206
[13]
Mesri G, Olson R. 1971. Mechanisms controlling the permeability of clays. Clays Clay Minerals, 19: 151-158
[14]
Moore D, Morrow C, Byerlee J. 1982. Use of swelling clays to reduce permeability and its potential application to nuclear waste repository sealing. Geophys Res Lett, 9: 1009-1012
[15]
Morrow C A, Shi L Q, Byerlee J B. 1981. Permeability and strength of San Andreas fault gouge under high pressure. Geophys Res Lett, 8: 325-328
[16]
Morrow C A, Zhang B C, Byerlee J D. 1986. Effective pressure law for permeability of Westerly granite under cyclic loading. J Geophys Res, 91: 3870-3876
[17]
Morris K, Shepperd C. 1982. The role of clay minerals in influencing porosity and permeability characteristics in the bridport sands of wytch farm, dorset. Clay Minerals, 17: 41-54
[18]
Rice J R. 1992. Fault stress states, pore pressure distributions, and the weakness of the San Andreas Fault. In: Evans B, Wong T F, eds. Earthquake Mechanics and Transport Properties of Rocks. London: Academic Press. 475-503
[19]
Rodwell W R, Nash P J. 1992. Mechanisms and modeling of gas migration from deep radioactive waste repositories. London: United Kingdom Nirex Ltd. 86
[20]
Rushing J A, Newsham K E, Lasswell P M, et al. 2004. Klinkenberg-corrected permeability measurements in tight gas sands: Steady-state versus unsteady-state techniques. SPE Annual Technical Conference and Exhibition, doi: 10.2118/89867-MS
[21]
Sibson R H. 1992. Implications of fault-valve behaviour for rupture nucleation and recurrence. Tectonophysics, 211: 283-293
Baptist O C, Sweeney S A. 1954. The effect of clays on the permeability of reservoir sands to waters of different saline contents. Coast Regional Conference on Clays and Clay. 505-515
[35]
Behnsen J, Faulkner D R. 2011. Water and argon permeability of phyllosilicate powders under medium to high pressure. J Geophys Res, 116: B12203
[36]
Bernabé Y, Brace W, Evans B. 1982. Permeability, porosity and pore geometry of hot-pressed calcite. Mech Mater, 1: 173-183
[37]
Brace W F, Walsh J B, Frangos W T. 1968. Permeability of granite under high pressure. J Geophys Res, 73: 2225-2236
[38]
Brown K M, Ransom B. 1996. Porosity corrections for smectite-rich sediments: Impact on studies of compaction, fluid generation, and tectonic history. Geology, 24: 843-846
[39]
Byerlee J. 1993. Model for episodic flow of high-pressure water in fault zones before earthquakes. Geology, 21: 303-306
[40]
Caine J S, Evans J P, Forster C B. 1996. Fault zone architecture and permeability structure. Geology, 24: 1025-1028
[41]
Cases J, Berend I, Francois M, et al. 1997. Mechanism of adsorption and desorption of water vapor by homoionic montmorillonite: 3. The Mg2+, Ca2+, Sr2+ and Ba2+ echanged forms. Clays Clay Minerals, 45: 8-22
[42]
Chen J Y, Yang X S, Duan Q B, et al. 2013a. Importance of thermochemical pressurization in the dynamic weakening of Longmenshan fault during the 2008 Wenchuan earthquake: Inference from experiments and modeling. J Geophys Res, 118: 4145-4169
[43]
Chen J Y, Yang X S, Ma S L, et al. 2013b. Mass removal and clay mineral dehydration/rehydration in carbonate-rich surface exposures of the 2008 Wenchuan Earthquake fault: Geochemical evidence and implications for fault zone evolution and coseismic slip. J Geophys Res, 118: 474-496
[44]
Elisabeth C, Jér？me C. 2005. Adhesion forces between wetted solid surfaces. J Chem Phys, 122: 1-9
[45]
Evans J P, Forster C B, Goddard J V. 1997. Permeability of fault-related rocks, and implications for hydraulic structure of fault zone. J Struc Geol, 19: 1393-1404
[46]
Faulkner D R, Rutter E H. 1998. The gas permeability of clay-bearing fault gouge at 20°C. In: Jones G., Fisher Q J, Knipe R J, eds. Faulting, Faulting, Faulting Sealing and Fluid Flow in Hydrocarbon Reservoirs. London Geol Soc Spec Publ, 147: 147-156
[47]
Israelachvili J N. 1992. Adhesion forces between surfaces in liquids and condensable vapours. Surf Sci Rep, 14: 109-159
[48]
Tanikawa W, Shimamoto T. 2009. Comparison of Klinkenberg-corrected gas permeability and water permeability in sedimentary rocks. Int J Rock Mech and Min Sci, 46: 229-238
[49]
Wu Y S, Pruess K, Persoff P. 1998. Gas flow in porous media with Klinkenberg effects. Transport Porous Media, 32: 117-137
[50]
Yang X S. Chen J Y, Duan Q B. 2011. Grain size distribution of fault rocks: Implication from natural gouges and high velocity friction experiments. American Geophysical Union, Fall Meeting. T32C-08
[51]
Zhang M, Takeda M, Esaki T, et al. 2001. Effects of confining pressure on gas and water permeabilities of rocks. Mat Res Soc Symp Proc. 663
[52]
Zoback D M, Byerlee D J. 1975. The effect of microcrack dilatancy on the permeability of westerly granite. J Geophys Res, 80: 752-757
