Moreton, Steven Grahame (2006): Major element compositions on glass shards of sediment core PC063; appendix I [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.351588, In supplement to: Moreton, SG (1999): Quaternary tephrochronology of the Scotia Sea and Bellingshausen Sea, Antarctica [dissertation]. Cheltenham and Gloucester College of Higher Education, 164 pp, MoretonSG_thesis_1999.pdf
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Coverage:
Latitude: -53.933300 * Longitude: -48.043300
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 2.64 m
Event(s):
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
280 data points
Data
1 Depth sed [m] | 2 SiO2 [%] | 3 TiO2 [%] | 4 Al2O3 [%] | 5 FeO [%] | 6 MnO [%] | 7 MgO [%] | 8 CaO [%] | 9 Na2O [%] | 10 K2O [%] | 11 Sample label |
---|---|---|---|---|---|---|---|---|---|---|
0.02 | 62.10 | 1.43 | 15.65 | 5.57 | 0.23 | 1.72 | 3.24 | 5.04 | 2.43 | PC063/1/2 |
0.02 | 63.17 | 1.39 | 15.44 | 5.48 | 0.16 | 1.38 | 2.83 | 5.35 | 2.81 | PC063/1/2 |
0.02 | 71.15 | 0.09 | 12.89 | 1.20 | 0.04 | 0.21 | 1.15 | 3.35 | 2.82 | PC063/1/2 |
0.02 | 72.74 | 0.15 | 11.54 | 0.97 | 0.05 | 0.16 | 0.76 | 2.73 | 4.17 | PC063/1/2 |
0.02 | 72.89 | 0.23 | 11.29 | 1.72 | 0.05 | 0.26 | 1.83 | 3.08 | 1.78 | PC063/1/2 |
0.02 | 73.25 | 0.21 | 11.23 | 1.92 | 0.05 | 0.21 | 1.85 | 3.10 | 1.92 | PC063/1/2 |
0.18 | 50.16 | 2.27 | 13.86 | 10.17 | 0.20 | 5.61 | 10.10 | 4.09 | 0.44 | PC063/1/18 |
0.18 | 51.97 | 2.81 | 14.70 | 11.67 | 0.24 | 4.02 | 7.38 | 4.97 | 0.69 | PC063/1/18 |
0.18 | 54.29 | 1.88 | 15.99 | 8.49 | 0.17 | 3.64 | 7.60 | 4.60 | 0.73 | PC063/1/18 |
0.18 | 54.30 | 2.51 | 16.51 | 8.83 | 0.16 | 3.00 | 7.44 | 5.23 | 0.54 | PC063/1/18 |
0.18 | 56.74 | 1.29 | 15.16 | 8.80 | 0.19 | 3.08 | 6.64 | 3.89 | 0.89 | PC063/1/18 |
0.18 | 59.22 | 0.60 | 14.22 | 9.37 | 0.40 | 0.05 | 0.95 | 7.99 | 4.40 | PC063/1/18 |
0.18 | 59.45 | 1.59 | 15.10 | 7.40 | 0.16 | 2.43 | 4.87 | 5.11 | 1.11 | PC063/1/18 |
0.18 | 59.57 | 1.20 | 15.55 | 7.19 | 0.20 | 2.25 | 5.17 | 3.95 | 1.64 | PC063/1/18 |
0.18 | 60.72 | 0.40 | 14.51 | 8.49 | 0.37 | 0.07 | 1.14 | 7.52 | 4.79 | PC063/1/18 |
0.18 | 61.27 | 0.73 | 14.66 | 7.59 | 0.31 | 0.31 | 1.39 | 6.45 | 4.79 | PC063/1/18 |
0.74 | 46.33 | 1.87 | 17.19 | 9.72 | 0.19 | 5.94 | 9.48 | 4.27 | 1.52 | PC063/2/20 |
0.74 | 47.55 | 2.46 | 16.70 | 8.23 | 0.19 | 4.90 | 9.15 | 4.39 | 2.39 | PC063/2/20 |
0.74 | 51.88 | 1.84 | 15.34 | 8.56 | 0.19 | 3.54 | 7.23 | 4.30 | 0.69 | PC063/2/20 |
0.74 | 52.63 | 1.59 | 16.54 | 7.32 | 0.19 | 4.13 | 7.95 | 4.09 | 0.57 | PC063/2/20 |
0.74 | 52.79 | 2.78 | 13.59 | 10.66 | 0.21 | 3.47 | 7.34 | 4.03 | 0.77 | PC063/2/20 |
0.74 | 66.34 | 0.28 | 12.89 | 1.51 | 0.05 | 0.23 | 1.21 | 2.80 | 4.67 | PC063/2/20 |
0.74 | 67.39 | 0.29 | 13.47 | 1.68 | 0.05 | 0.29 | 1.22 | 2.91 | 4.51 | PC063/2/20 |
0.74 | 68.00 | 0.27 | 13.22 | 1.69 | 0.07 | 0.30 | 1.31 | 2.89 | 4.44 | PC063/2/20 |
0.74 | 68.89 | 0.41 | 13.02 | 1.69 | 0.13 | 0.42 | 1.25 | 3.22 | 3.75 | PC063/2/20 |
2.64 | 46.56 | 1.95 | 17.10 | 9.53 | 0.21 | 5.84 | 9.55 | 4.47 | 1.39 | PC063/3/60 |
2.64 | 47.94 | 2.60 | 16.66 | 8.31 | 0.23 | 4.97 | 9.05 | 4.36 | 2.24 | PC063/3/60 |
2.64 | 53.18 | 1.67 | 15.89 | 8.15 | 0.20 | 3.94 | 7.77 | 4.95 | 0.66 | PC063/3/60 |