Barton, Charles E; Lackie, M; Peerdeman, F M (1993): (Table 2) Magnetic properties of ODP Site 133-820 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.786580, In supplement to: Barton, CE et al. (1993): Environmental control of magnetic properties of upper slope sediments near the Great Barrier Reef: results from Leg 133, Site 820. In: McKenzie, JA; Davies, PJ; Palmer-Julson, A; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 133, 543-562, https://doi.org/10.2973/odp.proc.sr.133.261.1993
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -16.637000 * Longitude: 146.303717
Date/Time Start: 1990-09-12T00:00:00 * Date/Time End: 1990-09-15T00:00:00
Minimum DEPTH, sediment/rock: 0.57 m * Maximum DEPTH, sediment/rock: 364.86 m
Event(s):
133-820 * Latitude: -16.637000 * Longitude: 146.303717 * Date/Time Start: 1990-09-12T00:00:00 * Date/Time End: 1990-09-15T00:00:00 * Elevation: -289.5 m * Penetration: 544.3 m * Recovery: 471 m * Location: Coral Sea * Campaign: Leg133 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 61 cores; 544.3 m cored; 0 m drilled; 86.5% recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Barton, Charles E | DSDP/ODP/IODP sample designation | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 3 | Zone | Zone | Barton, Charles E | |||
| 4 | Coercivity of remanence | Hcr | Oe | Barton, Charles E | ||
| 5 | Susceptibility, volume | kappa | µGs/Oe | Barton, Charles E | ||
| 6 | Natural remanent magnetization | NRM | mA/m | Barton, Charles E | ||
| 7 | Ratio | Ratio | Barton, Charles E | dl/dH = slope of the normalized IRM vs. field curve at high field | ||
| 8 | Koenigsberger ratio | Q-ratio | Oe | Barton, Charles E |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
174 data points
Data
| 1 Sample label | 2 Depth sed [m] | 3 Zone | 4 Hcr [Oe] | 5 kappa [µGs/Oe] | 6 NRM [mA/m] | 7 Ratio | 8 Q-ratio [Oe] |
|---|---|---|---|---|---|---|---|
| 133-820A-1H-1,58 | 0.57 | S | 456 | 6.9 | 8.23 | 1.19 | |
| 133-820A-1H-1,138 | 1.37 | S | 364 | 5.9 | 4.79 | 4.0 | 0.81 |
| 133-820A-1H-2,78 | 2.27 | A1 | 415 | 4.1 | 0.76 | 0.18 | |
| 133-820A-1H-3,38 | 3.37 | A1 | 380 | 5.4 | 3.45 | 10.0 | 0.63 |
| 133-820A-1H-4,78 | 5.27 | B1 | 440 | 14.7 | 21.99 | 1.49 | |
| 133-820A-1H-4,138 | 5.87 | B1 | 15.0 | 20.25 | 2.4 | 1.35 | |
| 133-820B-1H-4,12 | 4.61 | B1 | 363 | 10.8 | 19.98 | 1.85 | |
| 133-820B-1H-4,92 | 5.41 | B1 | 370 | 14.3 | 26.86 | 1.88 | |
| 133-820B-1H-5,132 | 7.31 | C1 | 245 | 25.4 | 5.99 | 2.0 | 0.23 |
| 133-820A-2H-4,17 | 11.86 | A2 | 410 | 6.5 | 0.69 | 0.11 | |
| 133-820A-3H-3,35 | 20.04 | A2 | 341 | 3.0 | 0.25 | 0.08 | |
| 133-820A-3H-3,95 | 20.64 | A2 | 367 | 4.0 | 0.27 | 5.0 | 0.07 |
| 133-820A-3H-7,17 | 25.86 | A2 | 375 | 3.4 | 0.06 | 7.0 | 0.02 |
| 133-820A-4H-3,138 | 30.57 | B2 | 395 | 16.0 | 8.43 | 6.0 | 0.53 |
| 133-820A-4H-4,37 | 31.06 | B2 | 440 | 18.5 | 15.39 | 0.83 | |
| 133-820A-4H-5,77 | 32.96 | C2 | 270 | 34.5 | 15.09 | 0.44 | |
| 133-820A-5H-7,59 | 45.28 | A | 328 | 4.4 | 0.54 | 0.12 | |
| 133-820A-7H-6,138 | 63.57 | D | 454 | 14.6 | 10.79 | 0.74 | |
| 133-820A-9H-1,138 | 75.07 | A | 343 | 3.5 | 0.47 | 0.13 | |
| 133-820A-10H-2,17 | 84.86 | A | 363 | 0.9 | 0.23 | 0.25 | |
| 133-820A-13H-6,97 | 120.16 | A | 334 | 3.5 | 0.44 | 0.12 | |
| 133-820B-18X-5,147 | 167.66 | A | 390 | 3.9 | 0.32 | 16.0 | 0.08 |
| 133-820B-20X-4,28 | 179.57 | A | 432 | 3.6 | 0.45 | 14.0 | 0.12 |
| 133-820B-21X-6,147 | 193.06 | A | 472 | 8.8 | 0.39 | 25.0 | 0.04 |
| 133-820B-28X-1,147 | 252.56 | A | 378 | 5.0 | 0.59 | 11.0 | 0.12 |
| 133-820B-38X-2,107 | 350.46 | A | 543 | 11.1 | 0.67 | 47.0 | 0.06 |
| 133-820B-40X-2,67 | 364.86 | A | 356 | 6.2 | 0.69 | 9.0 | 0.11 |