Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Ó Cofaigh, Colm; Graham, Alastair G C; Grobe, Hannes (2009): (Fig. 3a) Clay mineral content of sediment core JR104-GC366 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711157, 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: -72.845000 * Longitude: -82.615000
Date/Time Start: 2004-02-03T00:00:00 * Date/Time End: 2004-02-03T00:00:00
Minimum DEPTH, sediment/rock: 0.03 m * Maximum DEPTH, sediment/rock: 1.35 m
Event(s):
JR104-GC366 (GC366 CORE_NO 366) * Latitude: -72.845000 * Longitude: -82.615000 * Date/Time: 2004-02-03T00:00:00 * Elevation: -617.0 m * Recovery: 1.39 m * Location: Bellingshausen Sea, shallow part of trough in Eltanin Bay * Campaign: JR20040123 (JR104) * Basis: James Clark Ross * Method/Device: Gravity corer (GC) * Comment: smear slide, 2 core segments (0-41 cmbsf; 41-139 cmbsf)
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 [%] |
---|---|---|---|---|
0.03 | 18.8 | 55.8 | 21.6 | 3.8 |
0.12 | 17.3 | 54.0 | 22.8 | 5.9 |
0.22 | 0.8 | 67.6 | 27.4 | 4.3 |
0.28 | 0.5 | 68.4 | 26.5 | 4.6 |
0.38 | 0.8 | 67.7 | 27.4 | 4.1 |
0.48 | 0.9 | 68.9 | 26.4 | 3.7 |
0.58 | 0.5 | 68.9 | 26.1 | 4.5 |
0.68 | 0.5 | 62.5 | 31.5 | 5.5 |
0.78 | 0.5 | 68.8 | 27.0 | 3.7 |
0.91 | 1.0 | 71.8 | 23.7 | 3.5 |
1.02 | 0.2 | 69.6 | 26.5 | 3.6 |
1.14 | 0.6 | 70.1 | 25.8 | 3.5 |
1.27 | 0.4 | 69.1 | 26.8 | 3.8 |
1.35 | 1.1 | 68.1 | 27.1 | 3.8 |