Regular letterMagma storage conditions and control of eruption regime in silicic volcanoes: experimental evidence from Mt. Pelée
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2021, Earth-Science ReviewsCitation Excerpt :The chemical composition of materials erupted by Montagne Pelée has not changed significantly over the past 127 kyrs, except during the period 36–25 ka (Figs. 3, 4, 10). This lack of variation in the physical and chemical conditions of magma storage has been emphasized by experimental petrology (Martel et al., 1998), based on the comparison of natural product compositions from the last eruptions (P1, 1902–1905, 1929–1932; phenocrysts and glass) with experimental product compositions. The magma storage zone tapped during the past 25 kyrs activity of Montagne Pelée is composed of an andesitic magma (61–62 wt% SiO2, on average) that contains ~35–58 vol% of phenocrysts: 29–49 vol% plagioclase, 4–9 vol% orthopyroxene, 1–2 vol% magnetite, minor clinopyroxene, ilmenite and apatite, destabilized amphibole and olivine (Westercamp and Mervoyer, 1976; Gourgaud et al., 1989; Martel et al., 1998) embedded in a rhyolitic matrix glass (74–77 wt% SiO2; Martel et al., 2000).