Moreton, Steven Grahame (2006): Major element compositions on glass shards of sediment core E42-11; appendix I [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.351578, In supplement to: Moreton, SG (1999): Quaternary tephrochronology of the Scotia Sea and Bellingshausen Sea, Antarctica. PhD Thesis, Cheltenham and Gloucester College of Higher Education, 164 pp, MoretonSG_thesis_1999.pdf
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Coverage:
Latitude: -69.218333 * Longitude: -88.406667
Minimum DEPTH, sediment/rock: 0.20 m * Maximum DEPTH, sediment/rock: 0.20 m
Event(s):
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
160 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 |
---|---|---|---|---|---|---|---|---|---|---|
0.20 | 43.39 | 4.46 | 19.06 | 10.28 | 0.14 | 3.96 | 8.79 | 3.20 | 1.75 | E42-11 |
0.20 | 45.56 | 3.38 | 17.24 | 10.95 | 0.15 | 5.69 | 9.54 | 3.04 | 0.95 | E42-11 |
0.20 | 47.16 | 3.92 | 13.84 | 10.37 | 0.08 | 5.04 | 10.08 | 3.58 | 1.63 | E42-11 |
0.20 | 47.21 | 4.97 | 13.73 | 11.35 | 0.15 | 4.52 | 9.24 | 3.80 | 1.78 | E42-11 |
0.20 | 47.84 | 3.62 | 13.31 | 10.95 | 0.12 | 5.46 | 10.03 | 3.38 | 1.15 | E42-11 |
0.20 | 47.85 | 3.51 | 13.68 | 11.05 | 0.19 | 6.11 | 10.15 | 3.25 | 0.85 | E42-11 |
0.20 | 48.35 | 3.45 | 13.82 | 11.19 | 0.15 | 6.10 | 9.95 | 3.22 | 0.98 | E42-11 |
0.20 | 48.35 | 3.83 | 13.61 | 11.06 | 0.15 | 5.38 | 9.95 | 3.42 | 1.19 | E42-11 |
0.20 | 48.57 | 3.69 | 13.29 | 11.37 | 0.13 | 5.56 | 10.06 | 3.64 | 1.22 | E42-11 |
0.20 | 48.59 | 3.84 | 13.83 | 11.43 | 0.13 | 5.38 | 9.94 | 3.41 | 1.11 | E42-11 |
0.20 | 49.14 | 3.60 | 14.15 | 10.26 | 0.15 | 4.66 | 8.98 | 3.57 | 1.39 | E42-11 |
0.20 | 50.89 | 3.03 | 13.01 | 10.98 | 0.14 | 5.17 | 8.83 | 3.43 | 0.83 | E42-11 |
0.20 | 51.03 | 2.85 | 13.22 | 11.12 | 0.10 | 5.30 | 8.89 | 3.15 | 0.83 | E42-11 |
0.20 | 51.07 | 3.14 | 12.84 | 11.25 | 0.14 | 5.38 | 9.03 | 3.17 | 0.83 | E42-11 |
0.20 | 51.13 | 2.97 | 12.79 | 10.83 | 0.08 | 5.11 | 8.91 | 3.16 | 0.89 | E42-11 |
0.20 | 51.65 | 3.04 | 12.95 | 10.82 | 0.11 | 5.17 | 8.77 | 3.16 | 0.82 | E42-11 |