Franzese, Allison M; Hemming, Sidney R; Goldstein, Steven L (2009): (Table S10) Magnetic susceptibility for sediment core V24-216 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.832043, In supplement to: Franzese, AM et al. (2009): Use of strontium isotopes in detrital sediments to constrain the glacial position of the Agulhas Retroflection. Paleoceanography, 24(2), PA2217, https://doi.org/10.1029/2008PA001706
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Coverage:
Latitude: -37.320000 * Longitude: 24.767000
Date/Time Start: 1967-10-10T00:00:00 * Date/Time End: 1967-10-10T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 2.40 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Susceptibility | Suscept | sensor values | Franzese, Allison M | Magnetometer (MAG) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
110 data points
Data
1 Depth sed [m] | 2 Suscept [sensor values] |
---|---|
0.10 | 18 |
0.12 | 16 |
0.14 | 15 |
0.16 | 15 |
0.18 | 21 |
0.20 | 16 |
0.22 | 15 |
0.24 | 16 |
0.26 | 13 |
0.28 | 15 |
0.30 | 14 |
0.32 | 13 |
0.34 | 13 |
0.36 | 11 |
0.38 | 17 |
0.40 | 18 |
0.42 | 19 |
0.44 | 10 |
0.46 | 18 |
0.48 | 20 |
0.50 | 20 |
0.52 | 22 |
0.54 | 20 |
0.56 | 15 |
0.58 | 18 |
0.60 | 11 |
0.62 | 19 |
0.64 | 12 |
0.68 | 6 |
0.70 | 8 |
0.72 | 17 |
0.74 | 11 |
0.76 | 11 |
0.78 | 8 |
0.80 | 11 |
0.82 | 15 |
0.84 | 11 |
0.86 | 19 |
0.88 | 11 |
0.90 | 20 |
0.92 | 20 |
0.94 | 14 |
0.96 | 17 |
0.98 | 13 |
1.00 | 14 |
1.02 | 20 |
1.04 | 22 |
1.08 | 18 |
1.10 | 25 |
1.12 | 17 |
1.14 | 16 |
1.16 | 17 |
1.18 | 18 |
1.20 | 13 |
1.22 | 10 |
1.24 | 10 |
1.26 | 10 |
1.28 | 15 |
1.30 | 17 |
1.32 | 18 |
1.34 | 13 |
1.36 | 21 |
1.38 | 22 |
1.40 | 21 |
1.42 | 11 |
1.44 | 11 |
1.46 | 25 |
1.48 | 19 |
1.50 | 22 |
1.52 | 14 |
1.54 | 11 |
1.56 | 9 |
1.58 | 15 |
1.60 | 11 |
1.62 | 22 |
1.64 | 18 |
1.66 | 19 |
1.72 | 16 |
1.74 | 14 |
1.76 | 10 |
1.78 | 19 |
1.82 | 14 |
1.84 | 11 |
1.86 | 16 |
1.88 | 18 |
1.90 | 15 |
1.92 | 16 |
1.94 | 16 |
1.96 | 13 |
1.98 | 11 |
2.00 | 9 |
2.02 | 9 |
2.04 | 9 |
2.06 | 11 |
2.08 | 13 |
2.10 | 11 |
2.12 | 11 |
2.14 | 12 |
2.16 | 12 |
2.18 | 12 |
2.20 | 14 |
2.24 | 9 |
2.26 | 10 |
2.28 | 10 |
2.30 | 11 |
2.32 | 11 |
2.34 | 9 |
2.36 | 8 |
2.38 | 9 |
2.40 | 8 |