Acton, Gary D; Guyodo, Yohan; Brachfeld, Stefanie A (2002): (Table T2) Combined magnetostratigraphy of ODP Site 178-1096 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.737853, In supplement to: Acton, GD et al. (2002): Magnetostratigraphy of sediment drifts on the continental rise of West Antarctica (ODP Leg 178, Sites 1095, 1096, and 1101). In: Barker, PF; Camerlenghi, A; Acton, GD; Ramsay, ATS (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 178, 1-61, https://doi.org/10.2973/odp.proc.sr.178.235.2002
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -67.566817 * Longitude: -76.963517
Date/Time Start: 1998-02-27T00:00:00 * Date/Time End: 1998-02-27T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 589.59 m
Event(s):
178-1096 * Latitude: -67.566817 * Longitude: -76.963517 * Date/Time: 1998-02-27T00:00:00 * Elevation: -3152.3 m * Penetration: 1009 m * Recovery: 673.3 m * Location: South Pacific Ocean * Campaign: Leg178 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 90 cores; 811.2 m cored; 197.8 m drilled; 83% recovery
Comment:
DEPTH, sediment (m) is compsote depth (mcd)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Chronozone | Chronozone | Acton, Gary D | |||
| 3 | Polarity | Polarity | Acton, Gary D | reversal type: N>R = polarity of the field changed from normal to reversed, R>N = polarity of the field changed from reversed to normal | ||
| 4 | AGE | Age | ka BP | Geocode | ||
| 5 | Depth, composite top | Depth comp top | mcd | Acton, Gary D | ||
| 6 | Depth, composite bottom | Depth comp bot | mcd | Acton, Gary D | ||
| 7 | Sedimentation rate | SR | cm/ka | Acton, Gary D | ||
| 8 | Comment | Comment | Acton, Gary D | |||
| 9 | Comment 2 (continued) | Comm 2 | Acton, Gary D |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
104 data points
Data
| 1 Depth sed [m] | 2 Chronozone | 3 Polarity | 4 Age [ka BP] | 5 Depth comp top [mcd] | 6 Depth comp bot [mcd] | 7 SR [cm/ka] | 8 Comment | 9 Comm 2 |
|---|---|---|---|---|---|---|---|---|
| 0.00 | 0 | N | 0 | 0.00 | 0.00 | The mudline was not recovered in Holes 1096A and 1096C. | ||
| 56.10 | C1n (o) | R>N | 780 | 56.09 | 56.11 | 71.92 | Hole 1096B preferred. The reversal boundary is the same as identified by Shipboard Scientific Party (1999b), but the location of the boundary has been adjusted slightly. | |
| 145.51 | C2n (t) | N>R | 1770 | 145.36 | 145.66 | Reversal boundary not previously identified. | ||
| 155.50 | C2n (o) | R>N | 1950 | 146.86 | 155.76 | Chron 2An (o) is placed in the lower part of the coring gap (top of Core 178-1096B-19H). Reversal boundary not previously identified. | ||
| 172.87 | C2r.1n (t) | N>R | 2140 | 172.84 | 172.89 | 91.39 | Identification of chron and reversal boundaries is speculative; therefore, these reversal boundaries are not used in the sedimentation rate plots. Reversal boundary not previously identified. | |
| 173.92 | C2r.1n (o) | R>N | 2150 | 173.89 | 173.94 | 105.00 | Identification of chron and reversal boundaries is speculative; therefore, these reversal boundaries are not used in the sedimentation rate plots. Reversal boundary not previously identified. | |
| 220.63 | C2An.1n (t) | N>R | 2581 | 220.60 | 20.65 | 108.38 | Hole 1096C split-core results give the best estimate and agree within 10 cm with those from Hole 1096B. | The reversal boundary is the same as identified by Shipboard Scientific Party (1999b), but the location of the boundary has been adjusted slightly. Reversal boundary not previously identified. |
| 322.00 | C2An.1n (o) | R>N | 3040 | 321.74 | 324.53 | 220.86 | Subchron C2An.1n (o) is placed in the upper part of the coring gap. Reversal boundary not previously identified. | |
| 328.56 | C2An.2n (t) | N>R | 3110 | 328.53 | 328.58 | 93.64 | Reversal boundary not previously identified. | |
| 344.32 | C2An.2n (o) | R>N | 3220 | 344.29 | 344.34 | 143.27 | Reversal boundary not previously identified. | |
| 372.62 | C2An.3n (t) | N>R | 3330 | 372.59 | 372.64 | 257.27 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999b), but the location of the boundary has been adjusted slightly. | |
| 410.92 | C2An.3n (o) | R>N | 3580 | 410.69 | 411.14 | 153.20 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999b), but the location of the boundary has been adjusted slightly. | |
| 501.47 | C2Ar-1 (t) | Excursion | 501.44 | 501.49 | Excursion or possibly Subchron C3n.1n. Reversal boundary not previously identified. | |||
| 506.75 | C2Ar-1 (o) | Excursion | 506.72 | 506.77 | Excursion or possibly Subchron C3n.1n. Reversal boundary not previously identified. | |||
| 515.59 | C3n.1n (t) | N>R | 4180 | 514.08 | 517.09 | 174.45 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999b), but the location of the boundary has been adjusted slightly. | |
| 542.07 | C3n.1n (o) | R>N | 4290 | 541.99 | 542.14 | 240.73 | Reversal boundary is identical to that given by Shipboard Scientific Party (1999b). | |
| 559.24 | C3n.2n (t) | N>R | 4480 | 556.14 | 559.24 | 90.39 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999b), but the location of the boundary has been adjusted slightly. | |
| 589.59 | C3n.2n (o) | R>N | 4620 | 589.39 | 589.59 | 216.07 | Reversal boundary is identical to that given by Shipboard Scientific Party (1999b). |