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Smoothed or interpolated values are given in regT. S. Bowers, Gradient bridge, MA 02138 Corporation, 44 Brattle 2. 1 Volume Volume, or density, is usually measured. All other properties can be related by derivatives or integrals to volume. Detailed measurements of the volume of water at elevated pressures and temperatures have been made by (8) and (25). Water volumes are tabulated here in Table la-d from 0” to 2000°C and 1 bar to 250 Kbar based on data and tabulations of (15), (10) and (33). The work of (15) is based on a variety of measurements, including those of (25).

Hugoniots of Green River oil shale, in Proceedings of the 1977. Dianov, M. , N. A. Zlatin, G. S. Pugashev, and L. K. Rosomakho, 31 Shock compressibility of finely dispersed media, Sov. Tech. Phys. , 5, 285, 1979. Dick, R. , T. A. Weaver, and B. Olinger, Shock compression of the Webster dunite, EOS, 54,475, 1973. Dremin, A. , and G. A. Adadurov, Shock adiabatic for marble, Sov. Phys. Doklady, 4,970-973, 1959. Flanagan, T. , 1966. Gaffney, E. , 1973. Gault, D. , and E. D. Heitowit, The partition of energy for hypervelocity impact craters formed in rock, in Proceedings of the 6th Hypervelocity Impact Symposium, pp.

Geophys. , 70,381,1965. Wang, Z. and A. Nur, Wave velocities in hydrocarbon-saturated rocks: Experimental results, 96. 97. 98. , 1983. Frequency dependent ultrasonic properties of high-porosity sandstones, J. Geophys. Res.. S&,9493,1983. , Dispersion analysis of velocity and attenuation in Berea sandstone, J. Geophys. , 90, 183, 1985. , Estimates of velocity dispersion between seismic and ultrasonic frequencies, Geophysics, 51,6793,1986. Geophysics, 55,723, 1990. Wang, Z. and A. Nur, Seismic and Acoustic Velocities in Reservoir Rocks: Vol.

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