Ehrmann, Werner; Bloemendal, Jan; Hambrey, Mike J; McKelvey, Barrie C; Whitehead, Jason M (2003): Composition of the clay fraction at Mount Johnson [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.121628, 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: -71.533333 * Longitude: 67.566667
Date/Time Start: 1995-01-01T00:00:00 * Date/Time End: 1995-01-01T00:00:00
Minimum ELEVATION: 23 m a.s.l. * Maximum ELEVATION: 211 m a.s.l.
Event(s):
Mount_Johnson * Latitude: -71.533333 * Longitude: 67.566667 * Date/Time: 1995-01-01T00:00:00 * Location: Mount Johnson, 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 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
23 | AM 007 | 2 | 58 | 30 | 10.3 | 9.972 | 0.82 | 0.165 | 0.35 | 0.41 | 0.99 | 0.41 | 0.18 | 0.77 | 0.037 |
84 | AM 001 | 0 | 74 | 21 | 5.5 | 9.972 | 0.78 | 0.253 | 0.55 | 0.58 | 2.48 | 0.23 | 0.31 | 1.43 | 0.038 |
104 | AM 009 | 0 | 58 | 27 | 14.9 | 9.972 | 0.63 | 0.294 | 0.51 | 0.48 | 1.22 | 0.39 | 0.11 | 0.85 | 0.017 |
106 | AM 008 | 0 | 64 | 22 | 14.6 | 10.011 | 0.93 | 0.210 | 0.31 | 0.37 | 0.68 | 0.55 | 0.04 | 0.44 | 0.022 |
121 | AM 002 | 0 | 66 | 29 | 4.5 | 9.992 | 0.70 | 0.313 | 0.98 | 0.86 | 3.19 | 0.27 | 0.42 | 2.06 | 0.060 |
125 | AM 006 | 1 | 62 | 30 | 7.4 | 9.992 | 0.66 | 0.326 | 0.85 | 0.59 | 2.36 | 0.25 | 0.36 | 1.38 | 0.051 |
130 | AM 010 | 0 | 63 | 25 | 12.1 | 10.031 | 0.76 | 0.244 | 0.48 | 0.44 | 1.56 | 0.28 | 0.17 | 0.98 | 0.025 |
134 | AM 013 | 11 | 39 | 17 | 32.9 | 9.972 | 0.68 | 0.247 | 0.43 | 0.57 | 0.94 | 0.60 | 0.17 | 0.73 | 0.057 |
148 | AM 011 | 0 | 72 | 24 | 4.0 | 10.011 | 0.87 | 0.263 | 0.42 | 0.46 | 1.48 | 0.31 | 0.11 | 0.93 | 0.028 |
151 | AM 014 | 12 | 64 | 8 | 16.8 | 10.011 | 0.73 | 0.168 | 0.63 | 0.60 | 1.16 | 0.52 | 0.08 | 1.02 | 0.013 |
161 | AM 005 | 0 | 75 | 21 | 4.5 | 10.011 | 0.75 | 0.194 | 0.58 | 0.66 | 2.18 | 0.30 | 0.27 | 1.05 | 0.031 |
170 | AM 012 | 0 | 76 | 18 | 5.9 | 10.011 | 0.77 | 0.175 | 0.51 | 0.46 | 1.94 | 0.24 | 0.30 | 1.17 | 0.031 |
211 | AM 003 | 0 | 82 | 14 | 4.3 | 9.992 | 0.74 | 0.155 | 1.49 | 1.21 | 3.83 | 0.32 | 0.35 | 2.48 | 0.044 |