A model for intergranular pressure solution in open systems

[1]  Y. Leroy,et al.  Geometrical evolution of stressed and curved solid‐fluid phase boundaries: 2. Stability of cylindrical pores , 1994 .

[2]  H. Hardy,et al.  Seventh Symposium on Salt , 1993 .

[3]  Jacob N. Israelachvili,et al.  Adhesion forces between surfaces in liquids and condensable vapours , 1992 .

[4]  W. Heidug A thermodynamic analysis of the conditions of equilibrium at nonhydrostatically stressed and curved solid-fluid interfaces , 1991 .

[5]  M. Paterson,et al.  Experimental dissolution‐precipitation creep in quartz aggregates at high temperatures , 1991 .

[6]  A. Mullis The role of silica precipitation kinetics in determining the rate of quartz pressure solution , 1991 .

[7]  S. W. Brok,et al.  Experimental evidence for water weakening of quartzite by microcracking plus solution–precipitation creep , 1991, Journal of the Geological Society.

[8]  P. Schutjens Intergranular pressure solution in halite aggregates and quartz sands : an experimental investigation , 1991 .

[9]  Thomas Dewers,et al.  Differentiated structures arising from mechano-chemical feedback in stressed rocks , 1990 .

[10]  D. J. Barber,et al.  Deformation Processes in Minerals, Ceramics and Rocks , 1990 .

[11]  J. Cahn The Physical Chemistry of Stressed Solids , 1989 .

[12]  D. Houseknecht Intergranular Pressure Solution in Four Quartzose Sandstones , 1988 .

[13]  E. Rutter,et al.  Pressure solution in nature, theory and experiment , 1983, Journal of the Geological Society.

[14]  Rishi Raj,et al.  Creep in polycrystalline aggregates by matter transport through a liquid phase , 1982 .

[15]  P. Robin Pressure solution at grain-to-grain contacts , 1978 .

[16]  R. Boer,et al.  Pressure solution experiments on quartz sand , 1977 .

[17]  E. Rutter A Discussion on natural strain and geological structure - The kinetics of rock deformation by pressure solution , 1976, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[18]  M. Paterson Nonhydrostatic thermodynamics and its geologic applications , 1973 .

[19]  Robert L. Coble,et al.  A Model for Boundary Diffusion Controlled Creep in Polycrystalline Materials , 1963 .

[20]  P. K. Weyl Pressure solution and the force of crystallization: a phenomenological theory , 1959 .

[21]  J. C. Jaeger,et al.  Conduction of Heat in Solids , 1952 .

[22]  J. Willard Gibbs,et al.  The scientific papers of J. Willard Gibbs , 1907 .

[23]  J. Gibbs On the equilibrium of heterogeneous substances , 1878, American Journal of Science and Arts.

[24]  K. Milliken The Widespread Occurrence of Healed Microfractures in Siliciclastic Rocks: Evidence From Scanned Cathodoluminescence Imaging , 1994 .

[25]  S. Hickman,et al.  Chapter 10 Growth of Grain Contacts in Halite by Solution-transfer: Implications for Diagenesis, Lithification, and Strength Recovery , 1992 .

[26]  S. W. Brok An experimental investigation into the effect of water on the flow of quartzite , 1992 .

[27]  M. J. Grinfel'd,et al.  Thermodynamic methods in the theory of heterogeneous systems , 1991 .

[28]  C. Spiers,et al.  Densification of crystalline aggregates by fluid-phase diffusional creep , 1990 .

[29]  F. Lehner Thermodynamics of rock deformation by pressure solution , 1990 .

[30]  Raymond Siever,et al.  Pressure solution during diagenesis , 1989 .

[31]  W. Heidug,et al.  Thermodynamics of coherent phase transformations in nonhydrostatically stressed solids , 1985 .

[32]  J. Bataille,et al.  Nonequilibrium thermodynamics of pressure solution , 1984 .

[33]  R. M. Bowen Part I – Theory of Mixtures , 1976 .

[34]  S. Groot,et al.  Non-equilibrium thermodynamics , 1969 .

[35]  W. B. Kamb The thermodynamic theory of nonhydrostatically stressed solids , 1961 .