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- W2980523689 abstract "The hyperaluminous rocks from Vanoise occur on the western border of the basement of southern Vanoise (internal part of Briançonnais zone) and on the « zone houillère » (external part of Briançonnais) . The most characteristic assemblages are : 1) Pyrophyllite-diaspore-magnesiocarpholite ± chloritoïd ± paragonite ± chlorite + white mica. 2) Chloritoïd-white mica-paragonite ± chlorite. The cracks with a paragonite filling are abundant in all the hyperaluminous rocks and they suggest a sodic enrichment, the role of which is discussed as for the unstability of some minerals. Due to the coexistence of diaspore-pyrophyllite and the Si⁴ = 3,2 content of phengite the temperature and pressure of metamorphism was around 360° C and 5 kb." @default.
- W2980523689 created "2019-10-25" @default.
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- W2980523689 date "1977-01-01" @default.
- W2980523689 modified "2023-10-17" @default.
- W2980523689 title "Les associations minéralogiques des roches hyperalumineuses du Dogger de Vanoise. Leur signification dans le métamorphisme régional" @default.
- W2980523689 doi "https://doi.org/10.3406/bulmi.1977.7153" @default.
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