EMPA methods for major element analysis of volcanic glass in core samples from Macauley submarine volcano.
Abstract:
Summary of EMPA methods used in the analysis of volcanic glass samples from Macauley submarine volcano. Analysis of glass geochemistry was done to link deposits of large-scale sediment waves on the southwest flank of Macauley volcano with the 6.3 ka caldera-forming eruption and deposition of the on-land Sandy Bay Tephra.
How to cite this dataset:
Frey, S. E., Jutzeler, M., Matthieu, C., Rebecca, C. J., 2025. EMPA methods for major element analysis of volcanic glass in core samples from Macauley submarine volcano. , Version 1.0. Interdisciplinary Earth Data Alliance (IEDA).
https://doi.org/10.60520/IEDA/114226. Accessed 2025-11-10.
DOI Creation Date:
2025-11-03
Related
Publication(s):
Large-scale submarine sediment waves at Macauley caldera volcano: in-situ evidence of high-flux, syn-eruptive submarine transport, Accepted with Geochemistry, Geophysics, Geosystems.
License:
Creative Commons Attribution 4.0 International [CC-BY-4.0]
Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Kermadec arc, New Zealand
User Contributed Keyword(s):
Submarine eruption, cyclic steps, supercritical flow, volcanic density current
Data Available On:
2025-11-04
Related Information
References:
Smithsonian Volcano Number:
242021