Smith, James A; Hillenbrand, Claus-Dieter; Kuhn, Gerhard; Larter, Robert D; Graham, Alastair G C; Ehrmann, Werner; Moreton, Steven Grahame; Forwick, Matthias (2010): Clay mineral composition of sediment core JR141_VC422 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.755012, In supplement to: Smith, JA et al. (2011): Deglacial history of the West Antarctic Ice Sheet in the western Amundsen Sea Embayment. Quaternary Science Reviews, 30(5-6), 488-505, https://doi.org/10.1016/j.quascirev.2010.11.020
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Coverage:
Latitude: -73.617900 * Longitude: -113.709300
Date/Time Start: 2006-02-01T04:42:00 * Date/Time End: 2006-02-01T04:42:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 5.60 m
Event(s):
JR141_VC422 (VC422) * Latitude: -73.617900 * Longitude: -113.709300 * Date/Time: 2006-02-01T04:42:00 * Elevation: -833.0 m * Recovery: 5.76 m * Location: Amundsen Sea * Campaign: JR20060109 (JR141 JR150) * Basis: James Clark Ross * Method/Device: Vibro corer (VC)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Smectite | Sme | % | Smith, James A | X-ray diffraction TEXTUR, clay fraction | |
3 | Illite | Ill | % | Smith, James A | X-ray diffraction TEXTUR, clay fraction | |
4 | Chlorite | Chl | % | Smith, James A | X-ray diffraction TEXTUR, clay fraction | |
5 | Kaolinite | Kln | % | Smith, James A | X-ray diffraction TEXTUR, clay fraction | |
6 | Illite, integral width | Ill IW | d2Theta | Smith, James A | X-ray diffraction TEXTUR, clay fraction | |
7 | Illite 5Å/10Å Esquevin-index | Ill EI | Smith, James A | X-ray diffraction TEXTUR, clay fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
288 data points
Data
1 Depth sed [m] | 2 Sme [%] | 3 Ill [%] | 4 Chl [%] | 5 Kln [%] | 6 Ill IW [d2Theta] | 7 Ill EI |
---|---|---|---|---|---|---|
0.01 | 20.7 | 44.8 | 16.6 | 17.9 | 0.57 | 0.241 |
0.04 | 16.5 | 44.5 | 18.8 | 20.1 | 0.57 | 0.318 |
0.10 | 26.4 | 29.2 | 19.4 | 25.0 | 0.59 | 0.335 |
0.14 | 26.0 | 35.2 | 17.7 | 21.1 | 0.50 | 0.360 |
0.19 | 24.7 | 36.2 | 17.9 | 21.2 | 0.55 | 0.349 |
0.25 | 26.0 | 24.6 | 19.8 | 29.7 | 0.59 | 0.333 |
0.30 | 27.2 | 30.6 | 19.0 | 23.1 | 0.64 | 0.262 |
0.40 | 34.2 | 23.6 | 17.6 | 24.6 | 0.59 | 0.335 |
0.50 | 29.2 | 24.9 | 21.2 | 24.8 | 0.59 | 0.437 |
0.60 | 28.0 | 28.4 | 22.5 | 21.1 | 0.55 | 0.392 |
0.70 | 24.8 | 33.4 | 21.2 | 20.7 | 0.60 | 0.294 |
0.80 | 24.2 | 34.4 | 21.3 | 20.2 | 0.62 | 0.242 |
0.90 | 22.4 | 33.0 | 22.1 | 22.6 | 0.65 | 0.329 |
1.00 | 22.7 | 29.4 | 23.6 | 24.2 | 0.54 | 0.394 |
1.20 | 24.1 | 32.1 | 22.1 | 21.8 | 0.66 | 0.300 |
1.40 | 24.8 | 35.9 | 20.1 | 19.3 | 0.59 | 0.282 |
1.60 | 20.9 | 39.4 | 20.8 | 18.9 | 0.60 | 0.335 |
1.75 | 21.6 | 29.8 | 27.1 | 21.5 | 0.52 | 0.363 |
1.80 | 18.8 | 30.5 | 27.5 | 23.1 | 0.57 | 0.369 |
1.90 | 23.4 | 29.8 | 21.3 | 25.5 | 0.61 | 0.343 |
2.06 | 25.3 | 25.3 | 17.4 | 32.0 | 0.63 | 0.302 |
2.11 | 22.7 | 23.3 | 23.9 | 30.1 | 0.50 | 0.564 |
2.20 | 28.2 | 21.2 | 20.5 | 30.0 | 0.57 | 0.358 |
2.30 | 17.1 | 39.1 | 24.5 | 19.4 | 0.60 | 0.232 |
2.40 | 17.4 | 39.2 | 23.5 | 19.9 | 0.63 | 0.228 |
2.50 | 15.5 | 40.9 | 21.5 | 22.2 | 0.66 | 0.254 |
2.60 | 15.4 | 40.8 | 21.6 | 22.3 | 0.67 | 0.243 |
2.70 | 20.8 | 39.7 | 19.5 | 20.1 | 0.64 | 0.209 |
2.80 | 14.3 | 38.4 | 23.9 | 23.4 | 0.66 | 0.362 |
3.00 | 15.2 | 36.9 | 23.0 | 24.9 | 0.73 | 0.276 |
3.20 | 13.7 | 36.9 | 25.2 | 24.2 | 0.65 | 0.482 |
3.40 | 14.5 | 38.7 | 23.6 | 23.3 | 0.70 | 0.405 |
3.60 | 18.0 | 39.8 | 21.6 | 20.7 | 0.71 | 0.233 |
3.75 | 17.7 | 38.0 | 22.4 | 21.9 | 0.67 | 0.307 |
3.80 | 23.2 | 36.9 | 20.1 | 19.9 | 0.67 | 0.251 |
3.90 | 23.2 | 40.2 | 18.6 | 17.9 | 0.73 | 0.286 |
4.00 | 23.8 | 29.3 | 23.6 | 23.2 | 0.60 | 0.265 |
4.10 | 21.9 | 33.7 | 22.6 | 21.8 | 0.69 | 0.282 |
4.30 | 21.7 | 33.6 | 23.2 | 21.6 | 0.64 | 0.243 |
4.50 | 16.6 | 39.9 | 21.6 | 21.9 | 0.61 | 0.295 |
4.60 | 18.0 | 40.3 | 21.5 | 20.2 | 0.68 | 0.250 |
4.75 | 17.1 | 39.8 | 21.9 | 21.2 | 0.62 | 0.306 |
4.87 | 17.7 | 39.4 | 23.1 | 19.9 | 0.63 | 0.299 |
4.95 | 18.6 | 38.7 | 22.7 | 19.9 | 0.60 | 0.290 |
5.03 | 16.9 | 46.8 | 16.7 | 19.6 | 0.72 | 0.242 |
5.15 | 16.7 | 38.2 | 23.2 | 22.0 | 0.62 | 0.364 |
5.35 | 19.3 | 37.7 | 22.0 | 21.0 | 0.60 | 0.362 |
5.60 | 29.1 | 35.4 | 18.1 | 17.4 | 0.64 | 0.242 |