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Wawersik, 151-158, 1992. Horowitz, F. , Mixed state variable friction laws: Some implications for experiments and a stability analysis, Geophys. Res. , 15, 1243-1246, 1988. Horowitz, F. G. and A. Ruina, Slip patterns in a spatially homogeneous fault model, J. Geophys. , 94, 10279-10298, 1989. Ito, K. and M. Matsuzaki, Earthquakes as self-organized critical phenomena, J. Geophys. , 95, 6853-6860, 1990. Jaeger, J. , and N. G. W. Cook, Friction in granular materials, in Proc. , edited by A. M. Te'eni, 257-66, 1971.
E. & K. C. Nielsen, The effect of porosity on the brittle-ductile transition in sandstones, J. Geophys. , 96, 405-414, 1991. Shimamoto, T. and J. M. Logan, Velocity-dependent behaviors of simulated halite shear zones: An argument for silicates, in Earthquake Source Mechanics, edited by S. , Am. Geophys. , 37, 49-63, 1986. , and D. Sornette, Self-organized criticality and earthquakes, Europhys. , 9, 197-202, 1989. Stesky, R. , Rock friction - effect of confining pressure, temperature, and pore pressure, Pure App!.
F. Wong, Academic Press, 109-133, 1992. Y. -f. Wong, Department of Earth and Space Sciences, State University of New York at Stony Brook, Stony Brook, NY 11794-2100. Is the Dynamics of the Lithosphere Chaotic? Q. Li and E. Nyland Department of Physics, University of Alberta, Edmonton, Canada A region of the lithosphere might be considered a non-linear deterministic system described by as yet unknown differential equations. Even though the governing equations are unknown, a lithospheric phase portrait for such a region can be reconstructed from a single observable such as an earthquake catalog.