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|a Cassidy, M.
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|a Watt, S.F.L.
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|a Talling, P.J.
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|a Palmer, M.R.
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|a Edmonds, M.
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|a Jutzeler, M.
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|a Wall-Palmer, D.
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|a Manga, M.
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|a Coussens, M.
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|a Gernon, T.
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|a Taylor, R.N.
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|a Michalik, A.
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|a Inglis, E.
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|a Breitkreuz, C.
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|a Le Friant, A.
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|a Ishizuka, O.
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|a Boudon, G.
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|a McCanta, M.C.
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|a Adachi, T.
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|a Hornbach, M.J.
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|a Colas, S.L.
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|a Endo, D.
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|a Fujinawa, A.
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|a Kataoka, K.S.
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|a Maeno, F.
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|a Tamura, Y.
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|a Wang, F.
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|a Rapid onset of mafic magmatism facilitated by volcanic edifice collapse
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|c 2015-06-28.
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|z Get fulltext
|u https://eprints.soton.ac.uk/378158/1/grl53025.pdf
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|a 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 (6-10?km3) 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.
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|a Article
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