Nowaczyk, Norbert R (2006): Volume susceptibility of sediment core PS1520-13 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.351534
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Related to:
Nowaczyk, Norbert R (1991): Hochauflösende Magentostratigraphie spätquartärer Sedimente arktischer Meeresgebiete (High-resolution Magnetostratigraphy of late-Quarternary Arctic marine Sediments). Berichte zur Polarforschung = Reports on Polar Research, 78, 187 pp, https://doi.org/10.2312/BzP_0078_1991
Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 82.008333 * Longitude: 32.318333
Date/Time Start: 1987-07-14T00:00:00 * Date/Time End: 1987-07-14T00:00:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 0.94 m
Event(s):
PS1520-13 (GIK21520-13 PS11/310-13) * Latitude: 82.008333 * Longitude: 32.318333 * Date/Time: 1987-07-14T00:00:00 * Elevation: -2882.0 m * Penetration: 1.5 m * Recovery: 0.98 m * Location: Svalbard * Campaign: ARK-IV/3 (PS11) * Basis: Polarstern * Method/Device: Kasten corer (KAL)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Magnetic susceptibility, volume | kappa | 10-6 SI | Nowaczyk, Norbert R | Bartington MS2B bulk sensor 460 Hz | |
| 3 | Magnetic susceptibility, volume | kappa | 10-6 SI | Nowaczyk, Norbert R | Bartington MS2B bulk sensor 4600 Hz |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
36 data points
Data
| 1 Depth sed [m] | 2 kappa [10-6 SI] (Bartington MS2B bulk sensor 4...) | 3 kappa [10-6 SI] (Bartington MS2B bulk sensor 4...) |
|---|---|---|
| 0.05 | 209.30 | 209.30 |
| 0.10 | 209.30 | 193.20 |
| 0.15 | 257.60 | 225.40 |
| 0.20 | 257.60 | 225.40 |
| 0.25 | 241.50 | 225.40 |
| 0.31 | 257.60 | 257.60 |
| 0.36 | 257.60 | 241.50 |
| 0.41 | 257.60 | 241.50 |
| 0.46 | 273.70 | 257.60 |
| 0.51 | 257.60 | 225.40 |
| 0.56 | 257.60 | 241.50 |
| 0.61 | 241.50 | 241.50 |
| 0.66 | 273.70 | 257.60 |
| 0.74 | 225.40 | 225.40 |
| 0.79 | 257.60 | 257.60 |
| 0.84 | 273.70 | 257.60 |
| 0.89 | 241.50 | 225.40 |
| 0.94 | 257.60 | 257.60 |