Ehrmann, Werner; Bloemendal, Jan; Hambrey, Mike J; McKelvey, Barrie C; Whitehead, Jason M (2003): Composition of the clay fraction at Fisher Bench [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.121627, 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: -71.550000 * Longitude: 67.716667
Date/Time Start: 1995-01-01T00:00:00 * Date/Time End: 1995-01-01T00:00:00
Minimum ELEVATION: 3 m a.s.l. * Maximum ELEVATION: 282 m a.s.l.
Event(s):
Fisher_Bench * Latitude: -71.550000 * Longitude: 67.716667 * Date/Time: 1995-01-01T00:00:00 * Location: Fisher Bench, 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:
285 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 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
3 | AH 020 | 0 | 81 | 12 | 6.8 | 10.050 | 0.75 | 0.174 | 0.35 | 0.50 | 1.00 | 0.49 | 0.13 | 0.53 | 0.000 |
4 | AH 019/2 | 0 | 81 | 14 | 5.0 | 10.050 | 0.67 | 0.139 | 0.65 | 0.81 | 1.84 | 0.44 | 0.23 | 1.21 | 0.036 |
6 | AH 018/3 | 0 | 79 | 16 | 5.0 | 10.109 | 0.73 | 0.171 | 0.58 | 0.70 | 1.79 | 0.39 | 0.23 | 1.14 | 0.015 |
25 | AH 017/2 | 0 | 76 | 21 | 2.8 | 10.090 | 0.73 | 0.050 | 0.23 | 0.23 | 1.14 | 0.20 | 0.31 | 0.78 | 0.049 |
45 | AH 018/2 | 0 | 58 | 39 | 3.1 | 10.070 | 0.71 | 0.078 | 0.55 | 0.34 | 1.76 | 0.19 | 0.29 | 0.88 | 0.040 |
51 | AH 019/1 | 0 | 70 | 24 | 5.9 | 10.129 | 0.73 | 0.100 | 0.33 | 0.43 | 1.15 | 0.37 | 0.21 | 0.60 | 0.020 |
55 | AH 018/1 | 0 | 57 | 39 | 4.3 | 10.070 | 0.86 | 0.169 | 0.60 | 0.70 | 2.44 | 0.29 | 0.52 | 1.21 | 0.095 |
61 | AH 017/1 | 0 | 66 | 30 | 3.4 | 10.090 | 0.69 | 0.160 | 0.45 | 0.35 | 1.47 | 0.24 | 0.25 | 0.73 | 0.021 |
75 | AH 015 | 2 | 78 | 17 | 2.3 | 10.150 | 0.97 | 0.096 | 0.29 | 0.38 | 1.08 | 0.36 | 0.13 | 0.59 | 0.020 |
81 | AH 013 | 0 | 69 | 27 | 4.3 | 10.070 | 0.83 | 0.134 | 0.38 | 0.38 | 1.53 | 0.25 | 0.37 | 0.72 | 0.040 |
100 | AH 011 | 0 | 53 | 42 | 5.7 | 10.030 | 0.90 | 0.165 | 0.56 | 0.37 | 1.74 | 0.21 | 0.29 | 0.84 | 0.037 |
135 | AH 010 | 0 | 36 | 56 | 7.9 | 10.011 | 0.74 | 0.487 | 0.25 | 0.25 | 0.95 | 0.27 | 0.22 | 0.42 | 0.040 |
150 | AH 009 | 0 | 54 | 41 | 5.3 | 10.070 | 0.97 | 0.171 | 0.37 | 0.38 | 1.35 | 0.28 | 0.27 | 0.73 | 0.028 |
158 | AH 008 | 0 | 52 | 44 | 4.3 | 10.050 | 0.86 | 0.197 | 0.20 | 0.25 | 1.18 | 0.21 | 0.38 | 0.68 | 0.051 |
175 | AH 007 | 0 | 57 | 38 | 4.3 | 10.130 | 0.82 | 0.119 | 0.30 | 0.35 | 1.63 | 0.22 | 0.45 | 0.95 | 0.064 |
197 | AH 006 | 0 | 70 | 26 | 3.8 | 10.150 | 0.77 | 0.119 | 0.30 | 0.28 | 1.25 | 0.22 | 0.36 | 0.72 | 0.047 |
210 | AH 005 | 0 | 73 | 24 | 3.0 | 10.150 | 1.15 | 0.084 | 0.21 | 0.24 | 0.96 | 0.25 | 0.20 | 0.61 | 0.039 |
255 | AH 004 | 0 | 81 | 18 | 1.6 | 10.050 | 1.21 | 0.119 | 0.48 | 0.57 | 1.65 | 0.34 | 0.21 | 1.03 | 0.050 |
282 | AH 003/1 | 0 | 70 | 26 | 3.3 | 10.150 | 0.85 | 0.221 | 0.17 | 0.17 | 0.85 | 0.20 | 0.22 | 0.42 | 0.061 |