Moreton, Steven Grahame (2006): Major oxide geochemical compositions of glass shards from the southern Bellingshausen Sea tephra layers; Tab 3.6. PANGAEA, https://doi.org/10.1594/PANGAEA.352106, 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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Median Latitude: -68.635000 * Median Longitude: -90.373889 * South-bound Latitude: -69.218333 * West-bound Longitude: -91.883333 * North-bound Latitude: -67.940000 * East-bound Longitude: -88.406667
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 9.13 m
E11-21 * Latitude: -68.746667 * Longitude: -91.883333 * Elevation: -2240.0 m * Recovery: 2.5 m * Method/Device: Gravity corer (GC)
E11-22 * Latitude: -67.940000 * Longitude: -90.831667 * Elevation: -2264.0 m * Recovery: 12.8 m * Method/Device: Gravity corer (GC)
All iron calculated as FeO. Probe conditions: accelerating voltage 20kV, beam current 15nA, 1µm focused beam, 10 second count times
95 data points