Wallick, Brian P; Steiner, Maureen B (1992): (Table 1) Paleomagnetic analyses of ODP Hole 129-802A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.779249, In supplement to: Wallick, BP; Steiner, MB (1992): Paleomagnetism of Cretaceous basalts from the East Mariana Basin, western Pacific Ocean. In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 447-454, https://doi.org/10.2973/odp.proc.sr.129.134.1992
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 12.096300 * Longitude: 153.210300
Date/Time Start: 1989-12-25T10:15:00 * Date/Time End: 1990-01-04T17:20:00
Minimum DEPTH, sediment/rock: 500.29 m * Maximum DEPTH, sediment/rock: 553.83 m
Event(s):
129-802A * Latitude: 12.096300 * Longitude: 153.210300 * Date/Time Start: 1989-12-25T10:15:00 * Date/Time End: 1990-01-04T17:20:00 * Elevation: -5980.0 m * Penetration: 559.8 m * Recovery: 165.01 m * Location: North Pacific Ocean * Campaign: Leg129 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 62 cores; 559.8 m cored; 0 m drilled; 29.5 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Wallick, Brian P | DSDP/ODP/IODP sample designation | a = Samples in which the second AF step showed a rise in intensity; calculations of MDF and Q for these samples are based on the second or 2.5-mT AF step | |
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 3 | Lithologic unit/sequence | Unit | Wallick, Brian P | flow unit | ||
| 4 | NRM, Intensity | Inten (NRM) | mA/m | Wallick, Brian P | ||
| 5 | NRM, Inclination | Incl (NRM) | deg | Wallick, Brian P | ||
| 6 | NRM, median destructive field of natural remanent magnetization, alternating field | MDF (NRM) | mT | Wallick, Brian P | ||
| 7 | Intensity | Intensity | A/m | Wallick, Brian P | average stable | |
| 8 | Inclination | Incl | deg | Wallick, Brian P | average stable | |
| 9 | Magnetic susceptibility | MAGS | 10-6 SI | Wallick, Brian P | ||
| 10 | Koenigsberger ratio | Q-ratio | A/m | Wallick, Brian P |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
225 data points
Data
| 1 Sample label | 2 Depth sed [m] | 3 Unit | 4 Inten (NRM) [mA/m] | 5 Incl (NRM) [deg] | 6 MDF (NRM) [mT] | 7 Intensity [A/m] | 8 Incl [deg] | 9 MAGS [10-6 SI] | 10 Q-ratio [A/m] |
|---|---|---|---|---|---|---|---|---|---|
| 129-802A-57R-2,119 a | 500.29 | 1 | 16500 | -1.8 | 9.9 | 3.0 | -20.6 | 24900 | 19.8 |
| 129-802A-57R-3,32 | 509.92 | 1 | 28500 | -28.9 | 9.9 | 11.5 | -30.0 | 22700 | 37.6 |
| 129-802A-58R-1,6 | 516.06 | 2 | 19800 | -35.0 | 7.3 | 8.5 | -35.5 | 24200 | 24.5 |
| 129-802A-58R-2,15 | 517.65 | 2 | 3900 | -27.9 | 5.7 | 0.6 | -35.6 | 28600 | 4.1 |
| 129-802A-58R-2,61 | 518.11 | 2 | 6500 | -37.6 | 4.6 | 0.5 | -39.0 | 26500 | 7.3 |
| 129-802A-58R-2,13 | 518.84 | 4 | 15600 | -32.6 | 12.7 | 8.5 | -31.1 | 24700 | 18.9 |
| 129-802A-58R-3,6 | 519.00 | 5 | 8100 | -38.2 | 12.5 | 4.3 | -38.5 | 22900 | 10.6 |
| 129-802A-58R-3,58 | 519.58 | 5 | 11800 | -35.8 | 4.9 | 2.4 | -36.0 | 27700 | 12.8 |
| 129-802A-58R-4,51 a | 521.01 | 5 | 8900 | -17.2 | 8.6 | 2.8 | -19.3 | 25300 | 10.5 |
| 129-802A-58R-4,92 a | 521.42 | 5 | 600 | -21.9 | 8.3 | 2.9 | -21.0 | 24700 | 0.7 |
| 129-802A-59R-1,20 a | 525.60 | 7 | 3400 | 25.8 | 9.8 | 1.4 | -32.7 | 18600 | 5.5 |
| 129-802A-59R-1,119 a | 526.59 | 8 | 3800 | -46.1 | 9.1 | 1.5 | 40.8 | 17500 | 6.5 |
| 129-802A-59R-2,63 a | 527.53 | 10 | 16100 | 28.8 | 14.1 | 14.1 | -41.5 | 21500 | 22.4 |
| 129-802A-59R-2,135 a | 528.25 | 11 | 4700 | -5.1 | 9.7 | 3.1 | -28.8 | 25700 | 5.5 |
| 129-802A-59R-3,124 | 529.64 | 13 | 12200 | -46.9 | 9.9 | 4.1 | 47.4 | 22800 | 16.0 |
| 129-802A-60R-1,7 | 534.77 | 14 | 9600 | 43.7 | 9.3 | 2.4 | -45.0 | 22600 | 12.7 |
| 129-802A-60R-1,26 | 534.96 | 14 | 14800 | -42.3 | 12.3 | 0.4 | -31.3 | 20800 | 21.2 |
| 129-802A-61R-1,70 | 544.90 | 15 | 28800 | -34.4 | 8.7 | 7.3 | -34.3 | 22400 | 38.5 |
| 129-802A-61R-1,95 | 545.15 | 15 | 26800 | -32.3 | 8.9 | 7.9 | -32.9 | 18800 | 42.6 |
| 129-802A-61R-1,145 | 545.65 | 16 | 17700 | -30.9 | 8.5 | 4.4 | -31.5 | 26500 | 20.0 |
| 129-802A-62R-1,92 | 550.02 | 17 | 8400 | -33.5 | 5.3 | 1.8 | -34.6 | 27300 | 9.2 |
| 129-802A-62R-1,121 a | 551.81 | 17 | 4600 | -20.0 | 8.2 | 1.4 | -30.0 | 32400 | 4.3 |
| 129-802A-62R-2,27 | 552.37 | 17 | 5400 | -22.5 | 5.8 | 0.5 | 41.5 | 33300 | 4.8 |
| 129-802A-62R-2,64 | 552.74 | 17 | 10300 | -28.4 | 9.7 | 1.5 | -38.3 | 29600 | 10.4 |
| 129-802A-62R-3,23 | 553.83 | 17 | 11300 | -34.3 | 4.7 | 0.8 | 44.4 | 27000 | 12.5 |