REFERENCES

Aharonov, E., M. Spiegelman and P. Kelemen, 3D flow and reaction in porous media (with implications for the Earth's mantle, and sedimentary basins, J. Geophys. Res., in press, 1997a.

Aharonov, E., E.A. Tenthorey and C.H. Scholz, Precipitation sealing and diagenesis: 2) Theoretical Analysis, J. Geophys. Res., submitted, 1997b.

Aharonov, E. and D.H. Rothman, Growth of correlated pore-scale structures in sedimentary rocks: A dynamical model, J. Geophys. Res., 101, 2973-2987, 1996.

Angevine, C.L. and D.L. Turcotte, Porosity reduction by pressure solution: A theoretical model for quartz arenites, Geol. Soc. Am. Bull., 94, 1129-1134, 1983.

Barker, C., Aquathermal pressuring-role of temperature in development of abnormal-pressure zones, AAPG Bull., 56, 2068-2071, 1972.

Bernabé, Y., W.F. Brace, and B. Evans, Permeability, porosity and pore geometry of hot pressed calcite, Mech. Mat., 1, 173-183, 1982.

Bethke, C.M., Inverse hydrogeologic analysis of the distribution and origin of Gulf Coast-type geopressured zones, J. Geophys. Res., 91, 6536-6545, 1986.

Boer, R.B. De, P.J.C. Nagtegaal and E.M. Duyvis, Pressure solution experiments on quartz sand, Geochim. Cosmochim. Acta, 41, 257-264, 1977.

Boles, J.R. and S.G. Franks, Clay diagenesis in Wilcox sandstones of southwest Texas: Implications of smectite diagenesis on sandstone cementation, J. Sed. Petrol., 49, 55-70, 1979.

Bolton, E.W., A.C. Lasaga and D.M. Rye, A model for the kinetic control of quartz dissolution and precipitation in porous media flow with spatially variable permeability: Formulation and examples of thermal convection, J. Geophys. Res., 101, 22157-22187, 1996.

Bourbie, T. and B. Zingsner, Hydraulic and acoustic properties as a function of porosity in Fontainbleau sandstone. J. Geophys. Res., 90, 11524-11532, 1985.

Bredehoeft, J.D. and B.B. Hanshaw, On the maintenance of anomalous fluid pressures; 1, Thick sedimentary sequences, Geol. Soc. Am. Bull., 79, 1097-1106, 1968.

David, C., T.-f.Wong, W. Zhu and J. Zhang, Laboratory measurement of compaction-induced permeability change in porous rocks: Implications for the generation and maintenance of pore pressure excess in the crust. PAGEOPH, 143, 425-456,1994.

Dewers, T. and P. Ortoleva, Nonlinear dynamical aspects of deep basin hydrology: Fluid compartment formation and episodic fluid release, Am. J. Sci., 294, 713-755, 1994.

Divis, A.F. and J.A. McKenzie, Experimental authigenesis of phyllosilicates from feldspathic sands, Sedimentology, 22, 147-155, 1975.

Dove, P.M., Kinetic and thermodynamic controls on silica reactivity in weathering environments, In: Chemical Weathering Rates of Silicate Minerals, MSA Short Course, A.H. White, S.L. Brantley, eds. p. 235-290, 1995.

Elias, B.P. and A. Hajash, Jr., Changes in quartz solubility and porosity due to effective stress: An experimental investigation of pressure solution, Geology, 20, 451-454, 1992.

Fu, L., K.L. Milliken and J.M. Sharp Jr., Porosity and permeability variations in fractured and liesegang Breathitt sandstones (Middle Pennsylvanian), eastern Kentucky: diagenetic controls and implications for modeling dual-porosity systems, J. Hydrol., 154, 351-381, 1994.

Fuller, C.M. and J.M. Sharp Jr., Permeability and fracture patterns in extrusive volcanic rocks: Implications from the welded Santana Tuff, Trans-Pecos Texas, Geol. Soc. Am. Bull., 104, 1485-1496, 1992.

Gavrilenko, P. & Gueguen, Y. (1993): Fluid overpressures and pressure solution in the crust. Tectonophysics, 217, 91-110.

Gratier, J.P. and R. Guiguet, Experimental pressure solution-deposition on quartz grains: the crucial effect of the nature of the fluid, J. Structural Geol., 8, 845-856, 1986.

Hajash, A. & Bloom, M.A., Marine diagenesis of feldspathic sand: A flow-through experimental study at 200°C, 1 kbar, Chem. Geol., 89, 359-377, 1991.

Hickman, S.H. and B. Evans, Experimental pressure solution in halite: the effect of grain/interphase boundary structure, J. Geol. Soc. Lond., 148, 549-560, 1991.

Huang, W.-L. and J.M. Longo, Experimental studies of silicate-carbonate reactions-I. Applications to diagenesis, Appl. Geochem., 9, 501-522, 1994.

Hunt, J.M., Generation and migration of petroleum from abnormally pressured fluid compartments, AAPG Bull., 74, 1-12, 1990.

Lemée, C. and Y. Guéguen, Modelling of porosity loss during compaction and cementation of sandstones, Geology, 24, 875-878, 1996.

Lichtner, P.C., Continuum model for simultaneous chemical reactions and mass transport in hydrothermal systems, Geochim. Cosmochi. Acta, 49, 779-800, 1985.

Magara, K., Reevaluation of montmorillonite dehydration as cause of abnormal pressure and hydrocarbon migration, AAPG Bull., 59, 292-302, 1975.

Main, I.G., B.G.D., Smart, G.B., Shimmield, S.C., Elphick, B.R., Crawford and B.T. Ngwenya, The effects of combined changes in pore fluid chemistry and stress state on permeability in reservoir rocks: Preliminary results from analogue materials. In: North Sea Oil and Gas Reservoirs-III, p.357-370, Kluwer Academic publishers,1994.

Moody, J.B., J.E. Jenkins, and D. Meyer, An experimental investigation of the albitization of plagioclase. Can. Mineral., 23, 583-596, 1985.

Person, M., J.P Raffensperger, S. Ge and G. Garven, Basin-scale hydrogeologic modeling. Rev. Geophys., 34, 61-87, 1996.

Robin, P-Y.F. (1978): Pressure solution at grain-to-grain contacts. Geochim. Cosmochim. Acta, 42, 1383-1389.

Rutter, E.H., The kinetics of rock deformation by pressure solution, R. Soc. Lond. Phil. Trans., A283, 203-219, 1976.

Scholz, C.H., A. Léger, and S.L. Karner, Experimental diagenesis: Exploratory results. Geophys. Res. Lett., 22, 719-722, 1995.

Small, J.S., D.L. Hamilton, and S. Habesch, Experimental simulation of clay precipitation within reservoir sandstones 1: Techniques and examples, J. Sed. Petrol., 62, 508-519, 1992.

Sprunt, E.S. and A. Nur, Destruction of porosity through pressure solution, Geophysics, 42, 726-741, 1977.

Steefel, C.I. and A.C. Lasaga, A coupled model for transport of multiple chemical species and kinetic precipitation/dissolution reactions with application to reactive flow in single phase hydrothermal systems, Am. J. Sci., 294, 529-592, 1994.

Tada, R., R. Maliva and R. Siever, A new mechanism for pressure solution in porous quartzose sandstone, Geochim. Cosmochim. Acta, 51, 2295-2301, 1987.

Thompson, A.H., Fractals in rock physics, Annu. Rev. Earth Planet. Sci., 19, 237-262, 1991.

Thornton, E.C. and W.E. Seyfried, Jr., Sediment-sea-water interaction at 200 and 300°C, 500 bars pressure: The role of sediment composition in diagenesis and low-grade metamorphism of marine clay, Geol. Soc. Am. Bull., 96, 1287-1295, 1985.

Vavra, C.L. Mineral reactions and controls on zeolite-facies alteration in sandstone of the Central Transantarctic Mountains, Antarctica, J. Sed. Petrology, 59, 688-703, 1989.

Walder, J. & A. Nur, Porosity reduction and crustal pore pressure development. J. Geophys. Res., 89, 11539-11548, 1984.

Wolery, T.J., D.J. Sherwood, K.J. Jackson, J.M., Delaney, and I. Puigdomenech, EQ3/6: Status and applications, UCRL-91884. Lawrence Livermore Laboratory, University of California, 12 pp, 1984.

Zhang, S., M.S. Paterson, and S.F. Cox, Porosity and permeability evolution during hot isostatic pressing of calcite aggregates. J. Geophys. Res., 99, 15741-15760, 1994.

Zhu, W., C. David, and T-f. Wong, Network modeling of permeability evolution during cementation and hot isostatic pressing, J. Geophys. Res., 100, 15451-15464, 1995.

Zoback, M.D. and J.D. Byerlee, Effect of high-pressure deformation on permeability of Ottawa sand. AAPG Bull., 60, 1531-1542, 1976.

Zuddas, P. and G. Michard, Experimental mineral-fluid interaction in the Na-Ca-(Sr)-Al-Si system, Eur. J. Min., 5, 807-818, 1993.

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