The measurement of saturated rock electrical conductivity at lower crustal temperatures and high pressures

Abstract
A method has been developed to measure the electrical conductivity of electrolyte saturated rocks under simulated lower crustal temperatures and pressures. The method uses a metal sleeved sample, and a guard-ring electrode system has been used to minimise leakage currents through the sleeve. Seals were developed to mate the metallic and ceramic parts of the cell.

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