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We performed laboratory measurements of the electrical conductivity of a gabbro sample of the Oman ophiolite under high-pressures (0.6 and 0.8 GPa), high-temperatures (250-908°C), and dry conditions using a pistoncylinder type high-pressure apparatus. The studied gabbro can be regarded as a representative sample of the lower oceanic crustal rocks based on its previously reported elastic wave velocities. The gabbro sample was powdered and hot pressed, and then sintered prior to the electricaldoi:10.2465/jmps.171110 fatcat:gbl7w4jtjrh6jitlosqikihtqi