Ehrmann, Werner; Hillenbrand, Claus-Dieter; Smith, James A; Graham, Alastair G C; Kuhn, Gerhard; Larter, Robert D (2011): Clay mineral composition of sediment core PS69/295-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.755027, In supplement to: Ehrmann, W et al. (2011): Provenance changes between recent and glacial-time sediments in the Amundsen Sea embayment, West Antarctica: clay mineral assemblage evidence. Antarctic Science, 23(5), 471-486, https://doi.org/10.1017/S0954102011000320
Always quote citation above when using data! You can download the citation in several formats below.
Coverage:
Latitude: -74.478900 * Longitude: -104.101500
Date/Time Start: 2006-03-16T00:53:00 * Date/Time End: 2006-03-16T00:53:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 4.80 m
Event(s):
PS69/295-1 * Latitude: -74.478900 * Longitude: -104.101500 * Date/Time: 2006-03-16T00:53:00 * Elevation: -1151.0 m * Recovery: 4.86 m * Location: Amundsen Sea * Campaign: ANT-XXIII/4 (PS69) * Basis: Polarstern * Method/Device: Gravity corer (GC) * Comment: 5 core sections: 0-0.86, 0.86-1.86, 1.86-2.86, 2.86-3.86, 3.86-4.86 m
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Smectite | Sme | % | Ehrmann, Werner | X-ray diffraction TEXTUR, clay fraction | |
3 | Illite | Ill | % | Ehrmann, Werner | X-ray diffraction TEXTUR, clay fraction | |
4 | Chlorite | Chl | % | Ehrmann, Werner | X-ray diffraction TEXTUR, clay fraction | |
5 | Kaolinite | Kln | % | Ehrmann, Werner | X-ray diffraction TEXTUR, clay fraction | |
6 | Illite, integral width | Ill IW | d2Theta | Ehrmann, Werner | X-ray diffraction TEXTUR, clay fraction | |
7 | Illite 5Å/10Å Esquevin-index | Ill EI | Ehrmann, Werner | X-ray diffraction TEXTUR, clay fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
150 data points
Data
1 Depth sed [m] | 2 Sme [%] | 3 Ill [%] | 4 Chl [%] | 5 Kln [%] | 6 Ill IW [d2Theta] | 7 Ill EI |
---|---|---|---|---|---|---|
0.01 | 14.5 | 53.7 | 14.8 | 17.0 | 0.49 | 0.350 |
0.20 | 14.9 | 53.5 | 15.1 | 16.5 | 0.51 | 0.345 |
0.40 | 19.0 | 51.3 | 14.4 | 15.3 | 0.48 | 0.406 |
0.60 | 17.5 | 51.9 | 14.4 | 16.2 | 0.48 | 0.347 |
0.80 | 17.2 | 45.0 | 13.8 | 24.0 | 0.49 | 0.383 |
1.00 | 16.8 | 52.6 | 14.5 | 16.1 | 0.46 | 0.383 |
1.20 | 17.5 | 51.1 | 13.9 | 17.4 | 0.45 | 0.381 |
1.40 | 14.9 | 51.4 | 14.2 | 19.5 | 0.45 | 0.398 |
1.60 | 17.3 | 49.7 | 14.3 | 18.7 | 0.56 | 0.372 |
1.80 | 15.5 | 50.0 | 15.5 | 19.0 | 0.50 | 0.366 |
2.00 | 13.5 | 51.5 | 15.0 | 20.0 | 0.46 | 0.391 |
2.20 | 22.7 | 44.2 | 14.9 | 18.2 | 0.47 | 0.419 |
2.40 | 22.9 | 44.3 | 15.0 | 17.9 | 0.50 | 0.387 |
2.60 | 12.9 | 39.1 | 15.4 | 32.6 | 0.46 | 0.518 |
2.82 | 16.4 | 44.6 | 14.7 | 24.3 | 0.46 | 0.464 |
3.00 | 22.2 | 43.2 | 14.1 | 20.5 | 0.46 | 0.407 |
3.20 | 21.4 | 43.4 | 14.7 | 20.4 | 0.48 | 0.425 |
3.40 | 24.5 | 39.4 | 15.7 | 20.3 | 0.44 | 0.437 |
3.60 | 22.7 | 39.6 | 17.2 | 20.5 | 0.45 | 0.445 |
3.86 | 23.0 | 37.9 | 17.1 | 22.0 | 0.44 | 0.497 |
4.00 | 21.3 | 38.1 | 17.4 | 23.2 | 0.46 | 0.493 |
4.20 | 21.8 | 39.9 | 16.0 | 22.4 | 0.46 | 0.426 |
4.42 | 22.5 | 39.9 | 16.3 | 21.3 | 0.44 | 0.465 |
4.60 | 20.6 | 40.7 | 16.6 | 22.1 | 0.46 | 0.471 |
4.80 | 20.5 | 39.1 | 18.0 | 22.4 | 0.46 | 0.473 |