Supervolcano eruptions driven by melt buoyancy in large silicic magma chambers

Wim J. Malfait, Rita Seifert, Sylvain Petitgirard, Jean Philippe Perrillat, Mohamed Mezouar, Tsutomu Ota, Eizou Nakamura, Philippe Lerch, Carmen Sanchez-Valle

Research output: Contribution to journalArticle

62 Citations (Scopus)

Abstract

Super-eruptions that dwarf all historical volcanic episodes in erupted volume and environmental impact are abundant in the geological record. Such eruptions of silica-rich magmas form large calderas. The mechanisms that trigger these super-eruptions are elusive because the processes occurring in conventional volcanic systems cannot simply be scaled up to the much larger magma chambers beneath supervolcanoes. Over-pressurization of the magma reservoir, caused by magma recharge, is a common trigger for smaller eruptions, but is insufficient to generate eruptions from large supervolcano magma chambers. Magma buoyancy can potentially create sufficient overpressure, but the efficiency of this trigger mechanism has not been tested. Here we use synchrotron measurements of X-ray absorption to determine the density of silica-rich magmas at pressures and temperatures of up to 3.6 GPa and 1,950 K, respectively. We combine our results with existing measurements of silica-rich magma density at ambient pressures to show that magma buoyancy can generate an overpressure on the roof of a large supervolcano magma chamber that exceeds the critical overpressure of 10-40 MPa required to induce dyke propagation, even when the magma is undersaturated in volatiles. We conclude that magma buoyancy alone is a viable mechanism to trigger a super-eruption, although magma recharge and mush rejuvenation, volatile saturation or tectonic stress may have been important during specific eruptions.

Original languageEnglish
Pages (from-to)122-125
Number of pages4
JournalNature Geoscience
Volume7
Issue number2
DOIs
Publication statusPublished - Feb 2014

Fingerprint

magma chamber
buoyancy
volcanic eruption
magma
melt
overpressure
trigger mechanism
silica
recharge
geological record
caldera
roof
dike
environmental impact
saturation
tectonics
temperature

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)

Cite this

Malfait, W. J., Seifert, R., Petitgirard, S., Perrillat, J. P., Mezouar, M., Ota, T., ... Sanchez-Valle, C. (2014). Supervolcano eruptions driven by melt buoyancy in large silicic magma chambers. Nature Geoscience, 7(2), 122-125. https://doi.org/10.1038/ngeo2042

Supervolcano eruptions driven by melt buoyancy in large silicic magma chambers. / Malfait, Wim J.; Seifert, Rita; Petitgirard, Sylvain; Perrillat, Jean Philippe; Mezouar, Mohamed; Ota, Tsutomu; Nakamura, Eizou; Lerch, Philippe; Sanchez-Valle, Carmen.

In: Nature Geoscience, Vol. 7, No. 2, 02.2014, p. 122-125.

Research output: Contribution to journalArticle

Malfait, WJ, Seifert, R, Petitgirard, S, Perrillat, JP, Mezouar, M, Ota, T, Nakamura, E, Lerch, P & Sanchez-Valle, C 2014, 'Supervolcano eruptions driven by melt buoyancy in large silicic magma chambers', Nature Geoscience, vol. 7, no. 2, pp. 122-125. https://doi.org/10.1038/ngeo2042
Malfait WJ, Seifert R, Petitgirard S, Perrillat JP, Mezouar M, Ota T et al. Supervolcano eruptions driven by melt buoyancy in large silicic magma chambers. Nature Geoscience. 2014 Feb;7(2):122-125. https://doi.org/10.1038/ngeo2042
Malfait, Wim J. ; Seifert, Rita ; Petitgirard, Sylvain ; Perrillat, Jean Philippe ; Mezouar, Mohamed ; Ota, Tsutomu ; Nakamura, Eizou ; Lerch, Philippe ; Sanchez-Valle, Carmen. / Supervolcano eruptions driven by melt buoyancy in large silicic magma chambers. In: Nature Geoscience. 2014 ; Vol. 7, No. 2. pp. 122-125.
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