Supervolcano eruptions driven by melt buoyancy in large silicic magma chambers-Reference-Cited by-同舟云学术

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Supervolcano eruptions driven by melt buoyancy in large silicic magma chambers

Published:2014-01-05 Issue:2 Volume:7 Page:122-125
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

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

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo2042.pdf

Reference30 articles.

1. Mason, B. G., Pyle, D. M. & Oppenheimer, C. The size and frequency of the largest explosive eruptions on Earth. Bull. Volcanol. 66, 735–748 (2004).

2. Self, S. & Blake, S. Consequences of explosive supereruptions. Elements 4, 41–46 (2008).

3. Sparks, S. R. J. & Sigurdsson, H. Magma mixing: A mechanism for triggering acid explosive eruptions. Nature 267, 315–318 (1977).

4. Jellinek, A. M. & DePaolo, D. J. A model for the origin of large silicic magma chambers: Precursors of caldera-forming eruptions. Bull. Volcanol. 65, 363–381 (2003).

5. Sakamaki, T., Ohtani, E., Urakawa, S. & Suzuki, A. Measurements of hydrous peridotite magma density at high pressure using the X-ray absorption method. Earth Planet. Sci. Lett. 287, 293–297 (2009).

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