Hultzsch, Nadja (2007): Clay mineral composition of sediment core Lz1012 (Table A18) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.611260
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Related to:
Hultzsch, Nadja (2007): Lakustrine Sedimente als Archive des spätquartären Umweltwandels in der Amery-Oase, Ostantarktis (The Late Quaternary climatic and environmental history of Amery Oasis, East Antarctica). Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 545, 168 pp, https://doi.org/10.2312/BzPM_0545_2007
Project(s):
Permafrost Research (Periglacial Dynamics) @ AWI (AWI_PerDyn)
Coverage:
Latitude: -70.880500 * Longitude: 67.971710
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.26 m
Event(s):
Lz1012-1 * Latitude: -70.880500 * Longitude: 67.971710 * Lake water depth: 357 m * Recovery: 0.255 m * Location: Lake Radok, East Antarctica * Campaign: AmeryOasis2001/2002 * Basis: Sampling/drilling in lake * Method/Device: Gravity corer (GC)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Smectite | Sme | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
3 | Illite | Ill | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
4 | Kaolinite | Kln | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
5 | Chlorite | Chl | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
6 | Mica 5Å/10Å | Mica 5Å/10Å | Diekmann, Bernhard | Calculated | ||
7 | Quartz/Feldspar ratio | Qz/Fsp | Diekmann, Bernhard | Calculated | ||
8 | Plagioclase/Kalifeldspar ratio | Pl/Kfs | Diekmann, Bernhard | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
140 data points
Data
1 Depth sed [m] | 2 Sme [%] | 3 Ill [%] | 4 Kln [%] | 5 Chl [%] | 6 Mica 5Å/10Å | 7 Qz/Fsp | 8 Pl/Kfs |
---|---|---|---|---|---|---|---|
0.01 | 2.67 | 37.67 | 50.58 | 9.08 | 0.38 | 2.42 | 0.99 |
0.02 | 4.28 | 39.61 | 47.20 | 8.92 | 0.33 | 1.21 | 0.89 |
0.03 | 3.43 | 41.69 | 41.39 | 13.49 | 0.32 | ||
0.04 | 2.71 | 36.10 | 51.66 | 9.53 | 0.38 | ||
0.05 | 3.46 | 38.59 | 47.67 | 10.28 | 0.41 | ||
0.06 | 3.40 | 42.23 | 44.92 | 9.45 | 0.41 | 2.53 | 0.74 |
0.07 | 3.69 | 38.83 | 46.91 | 10.57 | 0.35 | ||
0.08 | 2.88 | 36.43 | 51.08 | 9.60 | 0.38 | ||
0.09 | 3.36 | 38.06 | 50.25 | 8.33 | 0.45 | ||
0.10 | 2.11 | 36.36 | 52.48 | 9.05 | 0.50 | 1.34 | 0.66 |
0.11 | 3.84 | 36.58 | 50.03 | 9.55 | 0.39 | 1.54 | 1.04 |
0.12 | 5.71 | 39.05 | 44.81 | 10.43 | 0.34 | 1.25 | 0.50 |
0.13 | 3.81 | 33.97 | 50.36 | 11.85 | 0.40 | ||
0.14 | 3.38 | 36.49 | 50.22 | 9.91 | 0.34 | ||
0.15 | 5.18 | 41.70 | 41.59 | 11.53 | 0.31 | 1.03 | 0.84 |
0.16 | 2.43 | 34.80 | 51.71 | 11.06 | 0.44 | ||
0.17 | 3.67 | 35.90 | 46.84 | 13.58 | 0.35 | ||
0.18 | 0.67 | 0.48 | |||||
0.20 | 3.34 | 34.12 | 47.54 | 15.01 | 0.34 | 0.64 | 0.45 |
0.21 | 5.80 | 38.93 | 45.19 | 10.08 | 0.31 | ||
0.22 | 3.29 | 36.66 | 49.98 | 10.07 | 0.46 | ||
0.23 | 4.08 | 38.23 | 47.82 | 9.87 | 0.37 | ||
0.24 | 5.79 | 36.41 | 47.35 | 10.44 | 0.27 | ||
0.25 | 5.47 | 41.48 | 44.46 | 8.59 | 0.33 | ||
0.26 | 6.52 | 41.62 | 43.38 | 8.48 | 0.28 | 1.59 | 0.79 |