Table T24. Results from APCT-3 temperature profiles, Site U1385.
| Core |
Minimum temperature (°C) |
Average temperature at mudline (°C) |
Depth DSF (m) |
In situ temperature (°C) |
|---|---|---|---|---|
| 339-U1385A- | ||||
| 4H | 3.34 | 3.37 | 30.0 | 5.06* |
| 7H | 3.45 | 3.69 | 58.5 | 5.83 |
| 10H | 3.45 | 3.80 | 87.0 | 7.05* |
| 13H | 3.37 | 3.56 | 115.5 | 8.02 |
| 339-U1385B- | ||||
| 4H | 3.48 | 3.59 | 34.6 | 4.78 |
| 7H | 3.52 | 3.65 | 63.1 | 5.77 |
| 10H | 3.56 | 3.67 | 91.6 | 7.11 |
| 13H | 3.49 | 3.55 | 120.1 | 7.95* |
| 339-U1385D- | ||||
| 4H | 3.40 | 3.64 | 35.4 | 4.89 |
| 7H | 3.49 | 3.71 | 60.9 | 5.47 |
| 10H | 3.22 | 3.30 | 89.4 | 6.91 |
| 13H | 3.23 | 3.48 | 117.9 | 7.91 |
| Average: | 3.42 | 3.58 | ||
* = unreliable measurement because of short measurement time and/or poor coupling with the formation. In situ temperatures were determined using TP-Fit software by Martin Heesemann. Thermal resistance was calculated from thermal conductivity data (see “Physical properties”) corrected for in situ conditions (see “Downhole measurements” section in the “Methods” chapter [Expedition 339 Scientists, 2013]).
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