Acton, Gary D; Guyodo, Yohan; Brachfeld, Stefanie A (2002): (Table T3) Magnetostratigraphy of ODP Hole 178-1101A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.737854, 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: -64.372200 * Longitude: -70.261180
Date/Time Start: 1998-03-18T10:30:00 * Date/Time End: 1998-03-18T10:30:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 209.38 m
Event(s):
178-1101A * Latitude: -64.372200 * Longitude: -70.261180 * Date/Time: 1998-03-18T10:30:00 * Elevation: -3279.7 m * Penetration: 217.7 m * Recovery: 215.75 m * Location: South Pacific Ocean * Campaign: Leg178 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 217.7 m cored; 0 m drilled; 99.1 % recovery
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 | (o) = onset, (t) = termination of a polarity chron | ||
| 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 | Sample code/label | Sample label | Acton, Gary D | DSDP/ODP/IODP sample designation | ||
| 8 | Sample code/label 2 | Sample label 2 | Acton, Gary D | DSDP/ODP/IODP sample designation | ||
| 9 | Sample comment | Sample comment | Acton, Gary D | |||
| 10 | Sedimentation rate | SR | cm/ka | Acton, Gary D | ||
| 11 | Comment | Comment | Acton, Gary D | |||
| 12 | Comment 2 (continued) | Comm 2 | Acton, Gary D |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
99 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 Sample label | 8 Sample label 2 | 9 Sample comment | 10 SR [cm/ka] | 11 Comment | 12 Comm 2 |
|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.00 | 0 | N | 0 | 0.00 | 0.00 | Top of 178-1101A-1H | The mudline is taken as 0-Ma sediment | ||||
| 55.05 | C1n (o) | R>N | 780 | 55.04 | 55.06 | 178-1101A-7H-5,135 | U-channel | 70.58 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. | ||
| 71.15 | C1r.1n (t) | N>R | 990 | 70.96 | 71.33 | 178-1101A-9H-3,145 | U-channel | 76.64 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. | ||
| 76.12 | C1r.1n (o) | R>N | 1070 | 75.95 | 76.29 | 178-1101A-9H | 178-1101A-10H | U-channel | 62.19 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. | |
| 81.61 | C1r.2r-1n (t) | N>R | 1201 | 80.96 | 82.26 | 178-1101A-10H-4,46 | U-channel | 41.91 | Identification of chron and reversal boundaries is speculative; therefore, these reversal boundaries are not used in the sedimentation rate plots. | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. | |
| 82.53 | C1r.2r-1n (t) | R>N | 1211 | 82.52 | 82.54 | 178-1101A-10H-5,33 | U-channel | 92.00 | Identification of chron and reversal boundaries is speculative; therefore, these reversal boundaries are not used in the sedimentation rate plots. | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. | |
| 121.25 | C2n (t) | N>R | 1770 | 121.24 | 121.26 | 178-1101A-14H-5,105 | U-channel | 64.47 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. | ||
| 126.96 | C2n (o) | R>N | 1950 | 126.95 | 126.97 | 178-1101A-15H-3,26 | U-channel | 31.72 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. | ||
| 136.20 | C2r.1n (t) | N>R | 2140 | 136.10 | 136.30 | 178-1101A-16H-2,150 | Split-core | 48.63 | Identification of chron and reversal boundaries is speculative; therefore, these reversal boundaries are not used in the sedimentation rate plots. | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. | |
| 136.63 | C2r.1n (o) | R>N | 2150 | 136.60 | 136.65 | 178-1101A-16H-3,43 | Split-core | 42.50 | Identification of chron and reversal boundaries is speculative; therefore, these reversal boundaries are not used in the sedimentation rate plots. | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. | |
| 165.98 | C2An.1n (t) | N>R | 2581 | 165.95 | 166.00 | 178-1101A-19X-3,138 | Split-core | 61.83 | The reversal boundary location is identical to that given by Shipboard Scientific Party (1999c). | ||
| 209.38 | C2An.1n (o) | R>N | 3040 | 209.35 | 209.40 | 178-1101A-24X-1,128 | Split-core | 94.55 | The reversal boundary is the same as identified by Shipboard Scientific Party (1999c), but the location of the boundary has been adjusted slightly. |