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Figure F44. A. Temperature data from the APCT-3, Cores 341-U1418A-4H, 7H, 10H, and 13H. An exponential decrease in temperature is expected for the time interval shown and was used to estimate ambient temperature. Data for the time interval t_i to t_f (solid circles) were used to estimate asymptotic temperature. B. Resulting geothermal gradient (60°C/km).

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