A cristobalite-bearing syenitic enclave in a drift pumice derived from the 2021 eruption of Fukutoku-Oka-no-Ba
Author:
Affiliation:
1. Japan Agency for Marine-Earth Science and Technology
2. School of Sustainable Design, University of Toyama
3. Necono-Wakuwaku Nature School
Publisher
Japan Association of Mineralogical Sciences
Link
https://www.jstage.jst.go.jp/article/jmps/119/1/119_231218/_pdf
Reference18 articles.
1. Carlut, J., Isambert, A., Carvallo, C., Garcia Da Fonseca, G., et al (2023) Rock magnetic analyses as a tool to investigate diversity in drift pumice clasts: an example from Japan’s 2021 Fukutoku-Oka-no-Ba (FOB) Eruption. Island Arc. doi:10.1111/iar.12507.
2. Casey, W.H., Westrich, H.R. and Holdren, G.R. (1991) Dissolution rates of plagioclase at pH = 2 and 3. American Mineralogist, 76, 211-217.
3. Elkins, L.T. and Grove, T.L. (1990) Ternary feldspar experiments and thermodynamic models. American Mineralogist, 75, 544-559.
4. Hamada, M., Hanyu, T., McIntosh, I.M., Tejada, M.L.G., et al (2023) Evolution of magma supply system beneath a submarine lava dome after the 7.3-ka caldera-forming Kikai-Akahoya eruption. Journal of Volcanology and Geothermal Research, 434, 107738.
5. Ikegami, F., McPhie, J., Carey, R., Mundana, R., et al (2018) The eruption of submarine rhyolite lavas and domes in the deep ocean-Havre 2012, Kermadec Arc. Frontiers in Earth Science, 6, 147.
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