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Figure F37. Thermal data, Hole C0008C. A. Thermal conductivity. B. Equilibrium temperatures (circles) and projected temperatures (line). The best-fit linear gradient to the equilibrium temperatures is 57°C/km. C. Temperature as a function of thermal resistance. The best-fit slope gives a heat flow value of 55 mW/m2 and a bottom water temperature of 1.8°C. CSF = core depth below seafloor.

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