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Bruno Scaillet
Researcher at University of Orléans
Publications - 196
Citations - 11613
Bruno Scaillet is an academic researcher from University of Orléans. The author has contributed to research in topics: Magma & Volcano. The author has an hindex of 61, co-authored 187 publications receiving 10108 citations. Previous affiliations of Bruno Scaillet include Centre national de la recherche scientifique & Blaise Pascal University.
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Evidence for mantle metasomatism by hydrous silicic melts derived from subducted oceanic crust
TL;DR: It is shown that the melting of basalt under both H2O-added and low-temperature conditions can yield extremely alkali-rich silicic liquids, the alkali content of which increases with pressure, suggesting that mantle metasomatism by slab-derived melt is a more common process than previously thought.
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The 15 June 1991 Eruption of Mount Pinatubo. I. Phase Equilibria and Pre-eruption P–T–fO2–fH2O Conditions of the Dacite Magma
Bruno Scaillet,Bernard W. Evans +1 more
TL;DR: In this paper, compositional zoning of hornblende is performed on a representative consistent either with an early crystallization event at ~400 MPa sample of the crystal-rich dacite ejected during the 15 June 1991 and 840-900°C, or with mixing events before eruption.
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Experimental Crystallization of Leucogranite Magmas
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Decadal to monthly timescales of magma transfer and reservoir growth at a caldera volcano
TL;DR: A study of pre-eruptive magmatic processes and their timescales using chemically zoned crystals from the ‘Minoan’ caldera-forming eruption of Santorini volcano, Greece, which occurred in the late 1600s bc, to provide insights into how rapidly large silicic systems may pass from a quiescent state to one on the edge of eruption.
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Carbonatite Melts and Electrical Conductivity in the Asthenosphere
Fabrice Gaillard,Mohammed Malki,Mohammed Malki,Giada Iacono-Marziano,Giada Iacono-Marziano,Michel Pichavant,Bruno Scaillet +6 more
TL;DR: It is shown that the conductivity of the oceanic asthenosphere can be explained by 0.1 volume percent of carbonatite melts on average, which agrees with the carbon dioxide content of mid-ocean ridge basalts.