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- W2758462985 abstract "Abstract The southern flank of the Maure-Vieille caldera of the Esterel massif of the Maritime Alps in southeastern France is remarkable for the large number of ignimbrite dikes in the series of alternating sedimentary and volcanic rocks of Permian age. Three types of dikes occur. The first is a rhyolitic rock poor in quartz and sanidine phenocrysts, but with abundant oriented laths consisting of a spherulitic quartz-potassic feldspar nucleus enclosed in an aureole of feldspar dusted with iron oxide. These 'fiammes' are devitrified fragments of pumice. The second type is of similar material but is brecciated in fragments cemented by a rhyolitic matrix. The third type is vitroclastic in structure with iron oxide inclusions, but completely devitrified. The rhyolite of the area is the same chemically as the ignimbrite, and the dikes of ignimbrite represent pyromagmatic fragmentation occurring in the conduits through which the rhyolite was erupted." @default.
- W2758462985 created "2017-10-06" @default.
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- W2758462985 date "1964-01-01" @default.
- W2758462985 modified "2023-09-26" @default.
- W2758462985 title "Existence de filons ignimbritiques au sud de la caldera de Maure-Vieille, Esterel oriental (Alpes-Maritimes)" @default.
- W2758462985 doi "https://doi.org/10.2113/gssgfbull.s7-vi.3.397" @default.
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