Moreton, Steven Grahame (2006): Major oxide geochemical compositions of glass shards from disseminated tephras above the megascopic ash from the Scotia Sea; Tab 4.3. PANGAEA, https://doi.org/10.1594/PANGAEA.354774, 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: -59.016250 * Median Longitude: -40.940825 * South-bound Latitude: -61.788300 * West-bound Longitude: -43.281700 * North-bound Latitude: -56.421700 * East-bound Longitude: -39.178300
Minimum DEPTH, sediment/rock: 0.04 m * Maximum DEPTH, sediment/rock: 1.62 m
GC027 * Latitude: -61.788300 * Longitude: -40.138300 * Elevation: -3470.0 m * Recovery: 4.7 m * Method/Device: Gravity corer (GC) * Comment: BAS core repository
GC037 * Latitude: -61.105000 * Longitude: -39.178300 * Elevation: -4025.0 m * Recovery: 4.1 m * Method/Device: Gravity corer (GC) * Comment: BAS core repository
All iron calculated as FeO. Probe conditions: accelerating voltage 20kV, beam current 15nA, 10 second count times
226 data points