Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Ó Cofaigh, Colm; Graham, Alastair G C; Grobe, Hannes (2009): (Fig. 3b) Clay mineral content of sediment core JR104-GC360 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711154, In supplement to: Hillenbrand, C-D et al. (2009): Clay mineral provenance of sediments in the southern Bellingshausen Sea reveals drainage changes of the West Antarctic Ice Sheet during the Late Quaternary. Marine Geology, 265(1-2), 1-18, https://doi.org/10.1016/j.margeo.2009.06.009
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Coverage:
Latitude: -71.995000 * Longitude: -76.551700
Date/Time Start: 2004-02-01T00:00:00 * Date/Time End: 2004-02-01T00:00:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 1.69 m
Event(s):
JR104-GC360 (GC360 CORE_NO 360) * Latitude: -71.995000 * Longitude: -76.551700 * Date/Time: 2004-02-01T00:00:00 * Elevation: -633.0 m * Recovery: 1.71 m * Location: Bellingshausen Sea, till sheet on N side of Ronne Entrance Trough * Campaign: JR20040123 (JR104) * Basis: James Clark Ross * Method/Device: Gravity corer (GC) * Comment: 2 core segments (0-72.5 cmbsf; 72.5-171 cmbsf), CC sample
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Smectite | Sme | % | Hillenbrand, Claus-Dieter | X-ray diffraction (XRD) | |
| 3 | Illite | Ill | % | Hillenbrand, Claus-Dieter | X-ray diffraction (XRD) | |
| 4 | Chlorite | Chl | % | Hillenbrand, Claus-Dieter | X-ray diffraction (XRD) | |
| 5 | Kaolinite | Kln | % | Hillenbrand, Claus-Dieter | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
56 data points
Data
| 1 Depth sed [m] | 2 Sme [%] | 3 Ill [%] | 4 Chl [%] | 5 Kln [%] |
|---|---|---|---|---|
| 0.05 | 27.1 | 45.1 | 22.6 | 5.2 |
| 0.15 | 26.3 | 43.7 | 24.1 | 5.9 |
| 0.25 | 14.8 | 46.9 | 30.9 | 7.4 |
| 0.35 | 10.4 | 50.7 | 32.1 | 6.7 |
| 0.45 | 33.1 | 27.7 | 26.5 | 12.7 |
| 0.55 | 28.9 | 27.2 | 29.8 | 14.0 |
| 0.65 | 30.3 | 28.5 | 28.3 | 12.9 |
| 0.80 | 31.6 | 28.5 | 26.1 | 13.8 |
| 0.95 | 26.3 | 27.5 | 30.1 | 16.1 |
| 1.10 | 28.3 | 29.1 | 28.3 | 14.3 |
| 1.25 | 23.8 | 32.2 | 28.7 | 15.4 |
| 1.40 | 26.2 | 28.0 | 30.1 | 15.7 |
| 1.54 | 28.3 | 26.8 | 29.8 | 15.1 |
| 1.69 | 28.0 | 26.5 | 27.9 | 17.5 |