Hailwood, Ernie A; Clement, Bradford M (1991): (Table 1) Polarity transitions of ODP Hole 114-699A. PANGAEA, https://doi.org/10.1594/PANGAEA.734970, 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
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -51.542000 * Longitude: -30.677000
Date/Time Start: 1987-03-20T10:45:00 * Date/Time End: 1987-03-26T15:29:00
Minimum DEPTH, sediment/rock: 10.59 m * Maximum DEPTH, sediment/rock: 464.65 m
Event(s):
114-699A * Latitude: -51.542000 * Longitude: -30.677000 * Date/Time Start: 1987-03-20T10:45:00 * Date/Time End: 1987-03-26T15:29:00 * Elevation: -3716.0 m * Penetration: 518.1 m * Recovery: 356.52 m * Location: South Atlantic Ocean * Campaign: Leg114 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 56 cores; 518.1 m cored; 0 m drilled; 68.8 % 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:
84 data points
Data
1 Depth sed [m] | 2 Std dev [±] | 3 Polarity |
---|---|---|
10.59 | 0.15 | N-R |
19.59 | 0.25 | R-N |
21.19 | 0.05 | N-R |
29.45 | 0.30 | R-N |
40.69 | 0.15 | N-R |
43.99 | ?0.05 | R-N |
53.61 | 0.53 | R-N |
58.01 | 0.07 | N-R |
60.86 | 0.21 | R-N |
62.39 | 0.05 | N-R |
68.84 | 0.10 | N-R |
70.29 | 0.05 | R-N |
87.57 | 0.27 | R-N |
91.17 | 0.63 | N-R |
92.49 | 0.15 | R-N |
94.47 | 0.03 | N-R |
115.35 | 0.45 | R-N |
116.22 | 0.18 | N-R |
118.09 | 0.05 | R-N |
118.49 | 0.15 | N-R |
119.24 | 0.10 | R-N |
127.69 | 0.15 | N-R |
137.09 | 0.05 | R-N |
142.74 | 0.10 | R-N |
143.05 | 0.10 | N-R |
143.84 | 0.10 | R-N |
145.73 | 0.08 | N-R |
146.21 | 0.04 | R-N |
156.14 | 0.10 | N-R |
166.95 | 0.75 | R-N |
182.69 | 0.35 | N-R |
189.34 | 0.10 | R-N |
192.55 | 0.10 | N-R |
193.05 | 0.10 | R-N |
195.55 | 0.10 | N-R |
197.00 | 0.05 | R-N |
198.35 | 1.55 | N-R |
208.09 | 0.25 | R-N |
216.05 | 0.75 | N-R |
284.55 | 0.86 | N-R |
434.68 | 0.20 | N-R |
464.65 | 0.63 | N-R |