Moreton, Steven Grahame (2006): Major element compositions on glass shards of sediment core E11-22; appendix I [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.351577, 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: -67.940000 * Longitude: -90.831667
Minimum DEPTH, sediment/rock: 9.13 m * Maximum DEPTH, sediment/rock: 9.13 m
Event(s):
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
270 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 |
---|---|---|---|---|---|---|---|---|---|---|
9.13 | 47.63 | 3.38 | 13.52 | 10.79 | 0.15 | 5.97 | 9.65 | 3.31 | 1.30 | E11-22/193 |
9.13 | 48.22 | 3.29 | 13.73 | 10.80 | 0.15 | 6.11 | 9.47 | 3.39 | 1.26 | E11-22/193 |
9.13 | 48.96 | 3.57 | 14.00 | 10.20 | 0.16 | 5.28 | 8.72 | 3.38 | 1.02 | E11-22/193 |
9.13 | 49.18 | 2.74 | 14.71 | 10.71 | 0.13 | 5.48 | 9.40 | 3.59 | 0.95 | E11-22/193 |
9.13 | 49.19 | 3.72 | 13.77 | 11.63 | 0.17 | 4.55 | 9.03 | 3.57 | 1.31 | E11-22/193 |
9.13 | 49.45 | 3.52 | 13.92 | 11.73 | 0.14 | 4.62 | 8.94 | 3.31 | 1.36 | E11-22/193 |
9.13 | 49.64 | 2.66 | 14.48 | 10.24 | 0.18 | 5.71 | 9.40 | 3.63 | 1.04 | E11-22/193 |
9.13 | 49.65 | 2.72 | 14.31 | 10.57 | 0.15 | 5.67 | 9.11 | 3.57 | 0.83 | E11-22/193 |
9.13 | 49.68 | 3.26 | 13.80 | 11.84 | 0.14 | 4.60 | 8.61 | 3.73 | 1.38 | E11-22/193 |
9.13 | 49.69 | 3.71 | 14.57 | 9.77 | 0.12 | 4.24 | 8.14 | 3.71 | 1.75 | E11-22/193 |
9.13 | 49.74 | 2.57 | 14.39 | 10.85 | 0.16 | 5.56 | 9.12 | 3.29 | 0.83 | E11-22/193 |
9.13 | 49.75 | 2.79 | 14.22 | 10.64 | 0.14 | 5.54 | 8.97 | 3.54 | 0.94 | E11-22/193 |
9.13 | 49.93 | 2.58 | 14.22 | 10.31 | 0.09 | 5.37 | 9.16 | 3.52 | 1.02 | E11-22/193 |
9.13 | 49.99 | 3.82 | 14.26 | 9.76 | 0.16 | 4.24 | 7.90 | 3.58 | 1.76 | E11-22/193 |
9.13 | 50.07 | 3.65 | 14.42 | 9.96 | 0.12 | 4.21 | 7.84 | 3.62 | 1.86 | E11-22/193 |
9.13 | 50.14 | 2.88 | 14.55 | 10.59 | 0.10 | 5.51 | 9.05 | 3.37 | 1.01 | E11-22/193 |
9.13 | 50.22 | 2.92 | 14.49 | 10.26 | 0.16 | 5.27 | 9.33 | 3.43 | 1.00 | E11-22/193 |
9.13 | 50.27 | 2.77 | 14.68 | 10.16 | 0.17 | 5.54 | 9.56 | 3.53 | 1.09 | E11-22/193 |
9.13 | 50.85 | 2.87 | 13.41 | 10.65 | 0.12 | 5.04 | 8.70 | 3.45 | 1.15 | E11-22/193 |
9.13 | 51.17 | 2.78 | 13.41 | 10.59 | 0.19 | 5.13 | 8.79 | 3.47 | 1.17 | E11-22/193 |
9.13 | 51.17 | 2.65 | 12.78 | 10.69 | 0.13 | 5.11 | 8.69 | 3.46 | 1.06 | E11-22/193 |
9.13 | 51.59 | 2.83 | 13.09 | 10.74 | 0.12 | 4.95 | 8.71 | 3.51 | 1.11 | E11-22/193 |
9.13 | 52.12 | 2.72 | 13.91 | 10.28 | 0.16 | 5.06 | 8.79 | 3.52 | 1.15 | E11-22/193 |
9.13 | 52.12 | 3.42 | 14.79 | 9.19 | 0.12 | 3.76 | 7.03 | 3.51 | 1.88 | E11-22/193 |
9.13 | 52.36 | 2.47 | 13.46 | 10.01 | 0.12 | 4.95 | 8.76 | 3.49 | 1.14 | E11-22/193 |
9.13 | 52.78 | 2.38 | 15.10 | 9.05 | 0.10 | 4.17 | 7.56 | 3.49 | 1.60 | E11-22/193 |
9.13 | 52.78 | 2.45 | 15.18 | 8.90 | 0.08 | 4.20 | 7.70 | 3.75 | 1.51 | E11-22/193 |