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 PS69/274-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.755021, 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
Always quote citation above when using data! You can download the citation in several formats below.
Coverage:
Latitude: -73.855900 * Longitude: -117.775700
Date/Time Start: 2006-03-07T02:48:00 * Date/Time End: 2006-03-07T02:48:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 4.40 m
Event(s):
PS69/274-1 * Latitude: -73.855900 * Longitude: -117.775700 * Date/Time: 2006-03-07T02:48:00 * Elevation: -1452.0 m * Recovery: 4.53 m * Campaign: ANT-XXIII/4 (PS69) * Basis: Polarstern * Method/Device: Gravity corer (GC) * Comment: 5 core sections: 0-0.53, 0.53-1.53, 1.53-2.53, 2.53-3.53, 3.53-4.53 m
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:
138 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 | 41.2 | 18.1 | 20.0 | 0.68 | 0.170 |
| 0.20 | 27.3 | 38.3 | 16.3 | 18.2 | 0.66 | 0.170 |
| 0.40 | 26.0 | 38.4 | 16.5 | 19.1 | 0.67 | 0.160 |
| 0.60 | 23.9 | 40.4 | 16.6 | 19.1 | 0.69 | 0.140 |
| 0.80 | 22.2 | 42.0 | 16.1 | 19.7 | 0.75 | 0.180 |
| 1.00 | 16.5 | 43.9 | 18.8 | 20.7 | 0.76 | 0.160 |
| 1.20 | 17.5 | 45.0 | 17.6 | 19.9 | 0.76 | 0.110 |
| 1.40 | 17.2 | 47.0 | 16.8 | 19.1 | 0.76 | 0.090 |
| 1.60 | 18.2 | 43.7 | 17.7 | 20.4 | 0.70 | 0.140 |
| 1.80 | 18.1 | 40.0 | 18.7 | 23.2 | 0.73 | 0.170 |
| 2.00 | 17.6 | 44.8 | 19.6 | 18.0 | 0.76 | 0.160 |
| 2.20 | 16.6 | 41.5 | 19.6 | 22.3 | 0.76 | 0.080 |
| 2.40 | 19.2 | 45.2 | 18.4 | 17.2 | 0.70 | 0.150 |
| 2.60 | 19.3 | 44.7 | 19.8 | 16.2 | 0.74 | 0.190 |
| 2.80 | 25.7 | 41.1 | 18.0 | 15.3 | 0.68 | 0.140 |
| 3.00 | 16.0 | 41.1 | 23.6 | 19.3 | 0.80 | 0.180 |
| 3.20 | 18.3 | 40.6 | 25.7 | 15.4 | 0.78 | 0.170 |
| 3.40 | 17.8 | 45.1 | 20.3 | 16.8 | 0.73 | 0.130 |
| 3.60 | 16.0 | 41.2 | 23.3 | 19.4 | 0.73 | 0.160 |
| 3.80 | 15.9 | 39.0 | 24.9 | 20.2 | 0.82 | 0.180 |
| 4.00 | 13.4 | 36.3 | 27.2 | 23.0 | 0.85 | 0.280 |
| 4.20 | 17.5 | 40.4 | 22.5 | 19.6 | 0.78 | 0.190 |
| 4.40 | 18.5 | 39.3 | 22.7 | 19.5 | 0.74 | 0.220 |