Thermal conductivity and diffusivity measurements on Alpine Fault rocks, New Zealand

Abstract

Drill core from Amethyst Tunnel, Hari Hari, Westland, New Zealand, and hand specimens from Stony Creek and Tarpot Creek, Westland, New Zealand, have been measured using Hot Disk in dry and saturated state at different temperatures (25 - 125 deggrees Celsius). Most were measured in bulk mode, some were also measured in anisotropic mode (radial and axial values) to obtain anisotropy coafficient. Two drill core samples were also measured in dry state at room tomperature using Thermal Conductivity Scanner

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