Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Ó Cofaigh, Colm; Graham, Alastair G C; Grobe, Hannes (2009): (Fig. 3d) Clay mineral content of sediment core JR104-GC357 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711151, 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: -71.766700 * Longitude: -80.110000
Date/Time Start: 2004-01-31T00:00:00 * Date/Time End: 2004-01-31T00:00:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 1.00 m
Event(s):
JR104-GC357 (GC357 CORE_NO 357) * Latitude: -71.766700 * Longitude: -80.110000 * Date/Time: 2004-01-31T00:00:00 * Elevation: -565.0 m * Recovery: 1.04 m * Location: Bellingshausen Sea, till sheet on shelf N of Smyley Island * Campaign: JR20040123 (JR104) * Basis: James Clark Ross * Method/Device: Gravity corer (GC) * Comment: 1 core segment (0-104 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:
52 data points
Data
| 1 Depth sed [m] | 2 Sme [%] | 3 Ill [%] | 4 Chl [%] | 5 Kln [%] |
|---|---|---|---|---|
| 0.02 | 24.2 | 44.0 | 24.8 | 7.0 |
| 0.07 | 34.3 | 36.8 | 23.1 | 5.8 |
| 0.12 | 39.6 | 29.9 | 24.1 | 6.4 |
| 0.18 | 36.7 | 32.1 | 23.8 | 7.5 |
| 0.24 | 34.4 | 32.8 | 25.3 | 7.5 |
| 0.30 | 30.5 | 34.5 | 26.8 | 8.2 |
| 0.40 | 31.0 | 32.3 | 27.9 | 8.8 |
| 0.50 | 31.1 | 32.2 | 27.7 | 8.9 |
| 0.60 | 30.5 | 35.2 | 25.4 | 8.9 |
| 0.70 | 35.5 | 33.3 | 23.6 | 7.6 |
| 0.80 | 35.5 | 32.4 | 24.5 | 7.6 |
| 0.90 | 38.1 | 30.5 | 24.3 | 7.2 |
| 1.00 | 35.9 | 30.4 | 25.6 | 8.1 |