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• W2078333271 endingPage "165" @default.
• W2078333271 startingPage "147" @default.
• W2078333271 abstract "The volcanic rocks of Mt. Pelée (Martinique) are predominantly composed of andesites; basic andesites and dacites are subordinate. The Mt. Pelée rocks have geochemical characteristics typical of island-arc calc-alkaline rocks. The chemical composition of the erupted material has not changed significantly during the past 100,000 y. This compositional uniformity with time is consistent with the model of McBirney (1980), which suggests that a magma chamber includes two zones — an upper graded stable part and a lower convecting part with approximately constant composition. Chemical variations within individual eruptions are ascribed to fractional crystallization, which probably was accompanied by a process leading to some homogenization of incompatible elements." @default.
• W2078333271 created "2016-06-24" @default.
• W2078333271 creator A5028217461 @default.
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• W2078333271 date "1985-10-01" @default.
• W2078333271 modified "2023-10-10" @default.
• W2078333271 title "Geochemistry of volcanic rocks from Mt. Pelée, Martinique" @default.
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• W2078333271 doi "https://doi.org/10.1016/0377-0273(85)90050-2" @default.
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