Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Ó Cofaigh, Colm; Graham, Alastair G C; Grobe, Hannes (2009): (Fig. 3f) Clay mineral content of sediment core JR104-GC371 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711160, 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: -70.653300 * Longitude: -84.540000
Date/Time Start: 2004-02-04T00:00:00 * Date/Time End: 2004-02-04T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 1.89 m
Event(s):
JR104-GC371 (GC371 CORE_NO 371) * Latitude: -70.653300 * Longitude: -84.540000 * Date/Time: 2004-02-04T00:00:00 * Elevation: -595.0 m * Recovery: 1.91 m * Location: Bellingshausen Sea, central axis of trough, outer shelf * Campaign: JR20040123 (JR104) * Basis: James Clark Ross * Method/Device: Gravity corer (GC) * Comment: smear slide, 2 core segments (0-92 cmbsf, 92-191 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:
72 data points
Data
| 1 Depth sed [m] | 2 Sme [%] | 3 Ill [%] | 4 Chl [%] | 5 Kln [%] |
|---|---|---|---|---|
| 0.01 | 23.7 | 47.3 | 22.2 | 6.8 |
| 0.06 | 25.7 | 42.3 | 23.9 | 8.1 |
| 0.11 | 37.8 | 36.2 | 19.6 | 6.4 |
| 0.16 | 35.5 | 34.7 | 23.4 | 6.3 |
| 0.21 | 39.2 | 33.2 | 21.4 | 6.1 |
| 0.26 | 35.0 | 35.9 | 22.9 | 6.2 |
| 0.35 | 29.4 | 37.6 | 25.4 | 7.6 |
| 0.45 | 27.9 | 34.8 | 29.3 | 8.0 |
| 0.59 | 29.2 | 36.8 | 26.0 | 8.0 |
| 0.73 | 28.6 | 35.0 | 28.0 | 8.4 |
| 0.87 | 27.0 | 38.4 | 27.0 | 7.5 |
| 1.00 | 28.9 | 35.5 | 27.9 | 7.7 |
| 1.15 | 28.4 | 34.9 | 27.7 | 9.0 |
| 1.30 | 28.6 | 33.9 | 28.8 | 8.7 |
| 1.45 | 27.6 | 36.5 | 27.0 | 8.9 |
| 1.60 | 28.2 | 36.4 | 27.9 | 7.6 |
| 1.75 | 29.4 | 36.3 | 25.0 | 9.3 |
| 1.89 | 28.3 | 37.5 | 26.9 | 7.3 |