Ehrmann, Werner; Bloemendal, Jan; Hambrey, Mike J; McKelvey, Barrie C; Whitehead, Jason M (2003): Composition of the clay fraction at Battye Glacier [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.121629, In supplement to: Ehrmann, W et al. (2003): Variations in the composition of the clay fraction of the Cenozoic Pagodroma Group, East Antarctica: implications for determining provenance. Sedimentary Geology, 161(1-2), 131-152, https://doi.org/10.1016/S0037-0738(03)00069-1
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Coverage:
Latitude: -70.083333 * Longitude: 67.966667
Date/Time Start: 1995-01-01T00:00:00 * Date/Time End: 1995-01-01T00:00:00
Minimum ELEVATION: 5 m a.s.l. * Maximum ELEVATION: 163 m a.s.l.
Event(s):
Battye_Glacier * Latitude: -70.083333 * Longitude: 67.966667 * Date/Time: 1995-01-01T00:00:00 * Location: Battye Glacier, East Antarctica * Campaign: AARE94/95 * Basis: Sampling on land * Method/Device: Geological sample (GEOS)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
195 data points
Data
1 Elevation [m a.s.l.] | 2 Sample label | 3 Sme [%] | 4 Ill [%] | 5 Chl [%] | 6 Kln [%] | 7 Ill 10Å [Å] | 8 Ill cryst [d2Theta] | 9 Ill EI | 10 Qz/std | 11 Kfs/std | 12 Pl/std | 13 Kfs/Pl | 14 Amp/std | 15 Pyrox/std | 16 Zeo/std |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
5 | AH 050 | 8 | 59 | 17 | 16.0 | 10.090 | 0.62 | 0.208 | 0.58 | 1.19 | 1.19 | 1.00 | 0.04 | 1.21 | 0.000 |
20 | AH 052 | 15 | 43 | 10 | 32.0 | 10.011 | 0.75 | 0.313 | 0.31 | 0.72 | 0.73 | 0.99 | 0.04 | 0.44 | 0.018 |
35 | AH 053 | 17 | 44 | 12 | 27.0 | 10.109 | 0.69 | 0.249 | 0.32 | 0.80 | 0.77 | 1.05 | 0.05 | 0.47 | 0.000 |
45 | AH055 | 7 | 52 | 15 | 27.0 | 10.109 | 0.63 | 0.181 | 0.48 | 1.05 | 1.10 | 0.95 | 0.03 | 0.96 | 0.021 |
45 | AH 056 | 16 | 52 | 7 | 26.0 | 10.011 | 0.69 | 0.272 | 0.75 | 1.20 | 1.28 | 0.94 | 0.00 | 0.67 | 0.052 |
63 | AH 058 | 26 | 32 | 10 | 32.0 | 10.011 | 0.69 | 0.342 | 0.26 | 0.47 | 0.46 | 1.03 | 0.08 | 0.23 | 0.000 |
84 | AH 059 | 15 | 58 | 7 | 20.0 | 10.090 | 0.75 | 0.102 | 0.38 | 0.74 | 0.81 | 0.91 | 0.03 | 0.59 | 0.043 |
90 | AH 060 | 18 | 59 | 8 | 15.0 | 10.109 | 0.88 | 0.082 | 0.55 | 1.24 | 1.34 | 0.93 | 0.03 | 1.14 | 0.021 |
98 | AH 061 | 21 | 41 | 8 | 30.0 | 10.070 | 0.92 | 0.209 | 0.32 | 0.68 | 0.66 | 1.04 | 0.01 | 0.54 | 0.022 |
105 | AH 062 | 18 | 34 | 6 | 42.0 | 10.070 | 0.82 | 0.286 | 0.38 | 0.73 | 0.75 | 0.97 | 0.04 | 0.46 | 0.041 |
125 | AH 063 | 24 | 48 | 8 | 19.0 | 10.070 | 0.74 | 0.169 | 0.51 | 0.89 | 1.00 | 0.89 | 0.19 | 0.70 | 0.022 |
154 | AH 065 | 9 | 70 | 5 | 16.0 | 10.050 | 0.85 | 0.218 | 0.42 | 0.77 | 0.89 | 0.86 | 0.04 | 0.54 | 0.040 |
163 | AH 066 | 5 | 75 | 5 | 15.0 | 10.070 | 0.97 | 0.153 | 0.21 | 0.31 | 0.40 | 0.78 | 0.03 | 0.23 | 0.028 |