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Nicole Métrich
Researcher at Institut de Physique du Globe de Paris
Publications - 118
Citations - 6458
Nicole Métrich is an academic researcher from Institut de Physique du Globe de Paris. The author has contributed to research in topics: Melt inclusions & Magma. The author has an hindex of 44, co-authored 115 publications receiving 5810 citations. Previous affiliations of Nicole Métrich include Paris Diderot University & National Institute of Geophysics and Volcanology.
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Journal ArticleDOI
Volatile Abundances in Basaltic Magmas and Their Degassing Paths Tracked by Melt Inclusions
Nicole Métrich,Paul J. Wallace +1 more
TL;DR: The abundances of CO2, H2O, S and halogens dissolved in basaltic magmas are strongly variable because their solubilities and ability to be fractionated in the vapor phase depend on several parameters such as pressure, temperature, melt composition and redox state as mentioned in this paper.
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Melt inclusion record of the conditions of ascent, degassing, and extrusion of volatile-rich alkali basalt during the powerful 2002 flank eruption of Mount Etna (Italy)
TL;DR: In this article, the authors decipher the origin and mechanisms of the second eruption from the composition and volatile (H2O, CO2, S, Cl) content of olivine-hosted melt inclusions in explosive products from its south flank vents.
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Crystallization Driven by Decompression and Water Loss at Stromboli Volcano (Aeolian Islands, Italy)
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2001 flank eruption of the alkali- and volatile-rich primitive basalt responsible for Mount Etna's evolution in the last three decades
TL;DR: A detailed study of the chemistry and dissolved volatile content of melt inclusions trapped in olivine crystals of unusual plagioclase-poor primitive basalt that was extruded during a highly explosive flank eruption in July-August 2001 is presented in this article.
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Conditions of Magma Storage, Degassing and Ascent at Stromboli: New Insights into the Volcano Plumbing System with Inferences on the Eruptive Dynamics
TL;DR: In this paper, an extensive dataset on major elements and volatiles (CO2, H2O, S and Cl) in olivine-hosted melt inclusions and embayments from pyroclasts emplaced during explosive eruptions of variable magnitude is presented.