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Progress in Earth and Planetary Science
Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

From: Simultaneous measurements of elastic wave velocities and electrical conductivity in a brine-saturated granitic rock under confining pressures and their implication for interpretation of geophysical observations

Fig. 3

a Compressional and b shear wave velocities in a dry rock sample AJG02. Velocities are shown as a function of confining pressure. Z-direction is parallel to the axis of the cylindrical sample. X- and Y-directions are perpendicular to Z-direction and mutually orthogonal. The letter for a compressional wave represents the propagation direction. The first letter for a shear wave is the oscillation direction, and the second letter is the propagation direction

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