Hultzsch, Nadja (2007): Clay mineral composition of sediment core Lz1007 (Table A16) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.611258
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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: -70.848250 * Longitude: 68.058500
Date/Time Start: 2001-01-14T00:00:00 * Date/Time End: 2001-01-14T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 2.02 m
Event(s):
Lz1007 * Latitude: -70.848250 * Longitude: 68.058500 * Date/Time: 2001-01-14T00:00:00 * Lake water depth: 74 m * Location: Lake Radok, East Antarctica * Campaign: AmeryOasis2001/2002 * Basis: Sampling/drilling in lake * Method/Device: Composite Core (COMPCORE)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Depth, composite | Depth comp | mcd | Diekmann, Bernhard | Intercore correlation | |
3 | Sample code/label | Sample label | Diekmann, Bernhard | |||
4 | Smectite | Sme | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
5 | Illite | Ill | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
6 | Kaolinite | Kln | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
7 | Chlorite | Chl | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
8 | Mica 5Å/10Å | Mica 5Å/10Å | Diekmann, Bernhard | Calculated | ||
9 | Quartz/Feldspar ratio | Qz/Fsp | Diekmann, Bernhard | Calculated | ||
10 | Plagioclase/Kalifeldspar ratio | Pl/Kfs | Diekmann, Bernhard | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
227 data points
Data
1 Depth sed [m] | 2 Depth comp [mcd] | 3 Sample label | 4 Sme [%] | 5 Ill [%] | 6 Kln [%] | 7 Chl [%] | 8 Mica 5Å/10Å | 9 Qz/Fsp | 10 Pl/Kfs |
---|---|---|---|---|---|---|---|---|---|
0.01 | 0.01 | Lz1007-1 | 1.33 | 32.80 | 57.75 | 8.12 | 0.40 | 5.42 | 0.40 |
0.06 | 0.06 | Lz1007-1 | 2.55 | 35.08 | 55.12 | 7.25 | 0.38 | 4.33 | 0.48 |
0.10 | 0.10 | Lz1007-1 | 1.31 | 35.19 | 55.72 | 7.79 | 0.36 | ||
0.11 | 0.11 | Lz1007-1 | 1.59 | 39.96 | 49.76 | 8.69 | 0.58 | 4.65 | 0.53 |
0.16 | 0.16 | Lz1007-1 | 1.96 | 33.21 | 57.47 | 7.36 | 0.41 | 4.33 | 0.42 |
0.17 | 0.17 | Lz1007-1 | 1.59 | 34.45 | 56.72 | 7.24 | 0.46 | 5.09 | 0.40 |
0.21 | 0.21 | Lz1007-1 | 2.35 | 37.50 | 52.00 | 8.15 | 0.42 | ||
0.26 | 0.26 | Lz1007-1 | 1.96 | 36.76 | 53.06 | 8.23 | 0.39 | 3.76 | 0.53 |
0.32 | 0.32 | Lz1007-2 | 0.00 | 37.63 | 51.42 | 10.95 | 0.38 | 2.79 | 1.05 |
0.42 | 0.42 | Lz1007-2 | 0.00 | 38.37 | 55.36 | 6.27 | 0.54 | ||
0.52 | 0.52 | Lz1007-2 | 0.76 | 43.27 | 48.53 | 7.44 | 0.41 | ||
0.62 | 0.62 | Lz1007-2 | 0.00 | 35.35 | 53.62 | 11.03 | 0.55 | ||
0.64 | 0.64 | Lz1007-2 | 0.00 | 37.84 | 51.53 | 10.63 | 0.52 | ||
0.66 | 0.66 | Lz1007-2 | 0.00 | 35.45 | 57.03 | 7.52 | 0.54 | 3.69 | 0.34 |
0.72 | 0.72 | Lz1007-2 | 0.00 | 37.72 | 54.49 | 7.79 | 0.54 | 3.64 | 0.82 |
0.82 | 0.82 | Lz1007-2 | 0.00 | 31.68 | 60.02 | 8.30 | 0.55 | ||
0.92 | 0.92 | Lz1007-2 | 0.32 | 27.41 | 65.31 | 6.97 | 0.53 | 4.19 | 0.32 |
1.02 | 1.02 | Lz1007-2 | 0.09 | 30.68 | 60.17 | 9.06 | 0.64 | ||
1.22 | 1.22 | Lz1007-2 | 0.00 | 32.42 | 59.07 | 8.51 | 0.61 | 4.89 | 0.27 |
1.26 | 1.26 | Lz1007-2 | 0.37 | 32.20 | 61.17 | 6.27 | 0.43 | ||
1.30 | 1.30 | Lz1007-2 | 0.37 | 30.89 | 62.27 | 6.46 | 0.45 | 4.73 | 0.44 |
1.36 | 1.36 | Lz1007-2 | 0.00 | 28.64 | 63.25 | 8.11 | 0.59 | ||
1.42 | 1.42 | Lz1007-2 | 0.00 | 29.90 | 60.49 | 9.61 | 0.62 | 5.63 | 0.56 |
1.46 | 1.46 | Lz1007-2 | 0.00 | 30.01 | 63.32 | 6.68 | 0.59 | 2.24 | 0.24 |
1.60 | 1.60 | Lz1007-2 | 0.46 | 30.18 | 60.95 | 8.41 | 0.45 | 7.40 | 0.34 |
1.80 | 1.80 | Lz1007-2 | 1.17 | 34.75 | 55.14 | 8.95 | 0.44 | 1.75 | 0.12 |
1.90 | 1.90 | Lz1007-2 | 0.12 | 26.24 | 64.56 | 9.08 | 0.57 | 1.84 | 0.33 |
2.02 | 2.02 | Lz1007-2 | 10.52 | 0.17 |