Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Ó Cofaigh, Colm; Graham, Alastair G C; Grobe, Hannes (2009): (Fig. 3c) Clay mineral content of sediment core JR104-GC359 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711153, 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: -71.718300 * Longitude: -76.038300
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: 1.47 m
Event(s):
JR104-GC359 (GC359 CORE_NO 359) * Latitude: -71.718300 * Longitude: -76.038300 * Date/Time: 2004-01-31T00:00:00 * Elevation: -685.0 m * Recovery: 1.53 m * Location: Bellingshausen Sea, ridge-groove province: ridge * Campaign: JR20040123 (JR104) * Basis: James Clark Ross * Method/Device: Gravity corer (GC) * Comment: 2 core segments (0-55.5 cmbsf; 55.5-153 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 [%] |
---|---|---|---|---|
0.02 | 30.7 | 36.9 | 25.1 | 7.3 |
0.11 | 35.0 | 34.7 | 21.8 | 8.6 |
0.20 | 33.4 | 30.4 | 28.8 | 7.4 |
0.30 | 20.9 | 35.8 | 32.1 | 11.2 |
0.40 | 25.3 | 37.3 | 28.2 | 9.3 |
0.50 | 10.2 | 36.7 | 42.4 | 10.7 |
0.57 | 9.8 | 33.0 | 47.5 | 9.7 |
0.67 | 12.3 | 38.5 | 39.5 | 9.6 |
0.77 | 13.6 | 35.7 | 37.3 | 13.4 |
0.87 | 12.8 | 37.2 | 38.2 | 11.8 |
1.02 | 13.0 | 36.9 | 38.0 | 12.1 |
1.17 | 14.0 | 39.1 | 34.4 | 12.5 |
1.32 | 12.7 | 35.6 | 38.2 | 13.5 |
1.47 | 10.6 | 37.2 | 38.8 | 13.5 |