Figure F36. Thermal data, Hole C0008A. A. Thermal conductivity. B. Equilibrium temperatures (circles) and projected temperatures (line). The best-fit linear gradient to the equilibrium temperatures is 51°C/km. C. Temperature as a function of thermal resistance. The best-fit slope gives a heat flow value of 52 mW/m2 and a bottom water temperature of 2.0°C. CSF = core depth below seafloor.
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