Rapid onset of mafic magmatism facilitated by volcanic edifice collapse
- Univ. of Southampton, Southampton (United Kingdom); Johannes Gutenberg Univ., Mainz (Germany)
- Univ. of Southampton, Southampton (United Kingdom); Univ. of Birmingham, Birmingham (United Kingdom)
- National Oceanography Centre, Southampton (United Kingdom)
- Univ. of Southampton, Southampton (United Kingdom)
- Univ. of Cambridge, Cambridge (United Kingdom)
- Plymouth Univ., Plymouth (United Kingdom)
- Univ. of California, Berkeley, CA (United States)
- Technische Univ. Bergakademie, Freiberg (Germany)
- Inst. de Physique du Globe de Paris, Paris (France)
- Geological Survey of Japan (AIST), Tsukuba (Japan)
- Tufts Univ., Medford, MA (United States)
- Yamagata Univ., Yamagata (Japan)
- Univ. of Texas, Austin, TX (United States)
- Univ. of Tsukuba, Tsukuba (Japan)
- Ibaraki Univ., Mito (Japan)
- Niigata Univ., Nishi-ku (Japan)
- Univ. of Tokyo, Bunkyo-ku (Japan)
- Japan Agency for Marine-Earth Science and Technology, Yokosuka (Japan)
- Chinese Academy of Sciences, Beijing (China)
Volcanic edifice collapses generate some of Earth's largest landslides. How such unloading affects the magma storage systems is important for both hazard assessment and for determining long-term controls on volcano growth and decay. Here we present a detailed stratigraphic and petrological analyses of volcanic landslide and eruption deposits offshore Montserrat, in a subduction zone setting, sampled during Integrated Ocean Drilling Program Expedition 340. A large (6-10km3) collapse of the Soufrière Hills Volcano at ~130 ka was followed by explosive basaltic volcanism and the formation of a new basaltic volcanic center, the South Soufrière Hills, estimated to have initiated <100 years after collapse. This basaltic volcanism was a sharp departure from the andesitic volcanism that characterized Soufrière Hills' activity before the collapse. Mineral-melt thermobarometry demonstrates that the basaltic magma's transit through the crust was rapid and from midcrustal depths. We suggest that this rapid ascent was promoted by unloading following collapse.
- Research Organization:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Organization:
- USDOE Office of Science (SC)
- Grant/Contract Number:
- AC02-05CH11231
- OSTI ID:
- 1512134
- Journal Information:
- Geophysical Research Letters, Vol. 42, Issue 12; ISSN 0094-8276
- Publisher:
- American Geophysical UnionCopyright Statement
- Country of Publication:
- United States
- Language:
- English
Web of Science
Geochemical and petrological diversity of mafic magmas from Mount St. Helens
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journal | January 2019 |
Multi-stage volcanic island flank collapses with coeval explosive caldera-forming eruptions
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journal | January 2018 |
Geochemical and petrological diversity of mafic magmas from Mount St. Helens
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text | January 2019 |
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