Table T26. Results from APCT-3 temperature profiles, Site U1386.
| Core |
Original depth (mbsf) |
Tidal sea level height* (m) |
Corrected depth (mbsf) |
In situ temperature (°C) |
Thermal resistance (m2K/W) |
|---|---|---|---|---|---|
| 339-U1389A- | |||||
| 4H | 32.8 | –1 | 33.9 | 14 | 27.06 |
| 7H | 61.3 | –1 | 62.4 | — | — |
| 10H | 89.8 | 0.1 | 89.8 | 15.29 | 71.51 |
| 339-U1389C- | |||||
| 2H | 19 | –0.6 | 19.7 | 13.7 | 15.42 |
| 5H | 39.5 | 0 | 39.6 | 14.21 | 30.98 |
| 8H | 68 | 1.5 | 66.6 | 14.85 | 52.29 |
| 339-U1389D- | |||||
| 3H | 24.5 | 0.8 | 23.8 | 14 | 19.25 |
| 6H | 53 | 1.2 | 51.9 | 14.35 | 38.73 |
| 9H | 75 | 0.8 | 74.3 | 14.8 | 58.36 |
* = +0.1 m tidal height when mudline Core 339-U1389A-1H was taken. 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” in the “Methods” chapter [Expedition 339 Scientists, 2012b]).
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