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Thin sections of a D2 strain gradient in paragneisses from the eastern part of the massif, close to Caladroy with a top-to-the-north kinematic. (A) low-strain deformation with local mylonites indicated by black arrows; (B) mylonitization generalized to the entire rock; (C) ultramylonitic texture with Qtz – Kfs – Bt – Sil assemblages (polarized normal light).
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