Abstract

The Evisa riebeckite granite massif of western Corsica is an alkaline hololeucocratic granite through which are scattered, with gradational contact, enclaves of a mesocratic riebeckite granite (lindinosite) with rare automorphic crystals of fluorite associated with clusters of riebeckite, and also included in it. The lindinosite is a facies of the Evisa granite.

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