Table T16. Remanent magnetization at 20 mT, Hole C0001F. (See table notes.)
| Core, section |
Declination (°) |
Inclination (°) |
α95 | N | k |
|---|---|---|---|---|---|
| 315-C0001F- | |||||
| 1H-1 | 332.7 | –48.5 | 09.8 | 17 | 014 |
| 1H-2 | 318.5 | –33.5 | 14.9 | 13 | 009 |
| 1H-3 | 358.1 | –42.5 | 14.8 | 15 | 008 |
| 1H-5 | 312.1 | –52.3 | 02.7 | 17 | 182 |
| 1H-6 | 312.1 | –52.6 | 04.6 | 11 | 098 |
| 1H-7 | 297.8 | –50.9 | 04.6 | 20 | 052 |
| 1H-8 | 295.7 | –35.1 | 10.0 | 07 | 037 |
| 1H-9 | 266.7 | –52.6 | 14.7 | 09 | 013 |
| 4H-4 | 346.0 | –49.3 | 15.8 | 22 | 005 |
| 5H-5 | 126.5 | 25.7 | 14.0 | 12 | 011 |
| 5H-8 | 022.8 | –55.3 | 11.1 | 22 | 009 |
| 5H-9 | 336.9 | –58.4 | 08.2 | 23 | 015 |
| 7H-3 | 142.3 | –40.6 | 16.0 | 18 | 006 |
| 7H-13 | 140.5 | –45.5 | 03.4 | 24 | 076 |
| 8H-3 | 340.4 | –39.4 | 13.7 | 16 | 008 |
| 8H-5 | 181.3 | 47.5 | 11.9 | 24 | 007 |
| 8H-6 | 170.5 | 45.5 | 04.3 | 16 | 074 |
| 8H-7 | 149.5 | 57.3 | 06.2 | 22 | 026 |
| 8H-8 | 144.6 | 38.0 | 10.5 | 04 | 078 |
| 9H-2 | 346.7 | 59.8 | 09.7 | 24 | 010 |
| 9H-3 | 337.7 | 63.2 | 13.0 | 12 | 012 |
| 9H-5 | 337.4 | 43.4 | 05.0 | 19 | 046 |
| 9H-6 | 319.5 | 54.0 | 04.9 | 24 | 038 |
| 10H-9 | 255.9 | 54.6 | 03.2 | 19 | 114 |
| 14H-1 | 204.2 | 57.9 | 17.5 | 09 | 010 |
| 14H-2 | 204.0 | 50.0 | 08.8 | 13 | 023 |
| 15H-1 | 197.0 | 51.8 | 09.3 | 22 | 012 |
| 15H-2 | 180.1 | 55.9 | 08.3 | 15 | 022 |
| 15H-3 | 165.8 | 50.9 | 13.3 | 12 | 012 |
| 19H-2 | 256.1 | 43.6 | 08.4 | 17 | 019 |
| 19H-4 | 229.2 | 44.4 | 12.3 | 14 | 011 |
Notes: Measurements made on archive halves where +x = vertical upward direction when the core is sitting with the single line at the bottom, +y = direction to the left along the split-core surface when looking upcore, and +z = downcore (see Fig. F18). Declination and inclination are for remanent magnetization at 20 mT. If inclination is positive (plain text), then declination needs to be restored to north (360°); if it is negative (bold text), it needs to be restored to the south (180°). α95 = radius of the 95% confidence cone centered around the mean paleomagnetic direction. N = number of measurements (= intervals). k = Fisher or precision parameter.
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