Hailwood, Ernie A; Clement, Bradford M (1991): (Table 2) Polarity transitions of ODP Hole 114-700B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.734971, In supplement to: Hailwood, EA; Clement, BM (1991): Magnetostratigraphy of sites 699 and 700, East Georgia Basin. In: Ciesielski, PF; Kristoffersen, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 114, 337-357, https://doi.org/10.2973/odp.proc.sr.114.155.1991
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -51.533000 * Longitude: -30.278100
Date/Time Start: 1987-03-27T22:45:00 * Date/Time End: 1987-04-03T12:45:00
Minimum DEPTH, sediment/rock: 48.45 m * Maximum DEPTH, sediment/rock: 430.95 m
Event(s):
114-700B * Latitude: -51.533000 * Longitude: -30.278100 * Date/Time Start: 1987-03-27T22:45:00 * Date/Time End: 1987-04-03T12:45:00 * Elevation: -3612.0 m * Penetration: 489 m * Recovery: 245.19 m * Location: South Atlantic Ocean * Campaign: Leg114 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 53 cores; 472.1 m cored; 0 m drilled; 51.9 % recovery
Comment:
Transitions interpolated within coring or sampling gaps can be identified from the associated large range of uncertainty. Boundaries of thin or otherwise poorly defined polarity intervals are indicated by a query
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Standard deviation | Std dev | ± | Hailwood, Ernie A | ||
| 3 | Polarity | Polarity | Hailwood, Ernie A | downward change in polarity |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
56 data points
Data
| 1 Depth sed [m] | 2 Std dev [±] | 3 Polarity |
|---|---|---|
| 48.45 | ?0.35 | N-R |
| 55.76 | ?0.39 | R-N |
| 68.60 | 1.50 | N-R |
| 152.01 | 0.47 | R-N |
| 164.16 | 5.51 | N-R |
| 190.86 | 0.52 | N-R |
| 267.19 | ?0.45 | R-N |
| 268.42 | ?0.78 | N-R |
| 299.13 | 0.13 | R-N |
| 314.76 | 0.20 | N-R |
| 315.16 | 0.10 | R-N |
| 316.76 | 0.10 | N-R |
| 316.96 | 0.10 | R-N |
| 318.16 | 0.10 | N-R |
| 318.84 | 0.38 | R-N |
| 327.31 | 0.16 | R-N |
| 333.29 | 0.04 | N-R |
| 337.72 | 0.62 | R-N |
| 344.22 | 1.92 | N-R |
| 357.75 | 0.10 | R-N |
| 359.45 | 0.10 | N-R |
| 360.95 | 0.10 | R-N |
| 369.80 | ?0.15 | N-R |
| 376.45 | 0.10 | N-R |
| 384.82 | 0.14 | R-N |
| 397.64 | 0.46 | R-N |
| 407.45 | 0.10 | N-R |
| 430.95 | 0.10 | R-N |