Fig. 2
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Structural map on the eastern half of the Montagne Noire gneiss dome showing the orientation of planar fabrics and interpreted foliation trajectories (modified from Rabin et al., 2015). The stereogram shows the preferential orientation of the quartz-bearing dykes that cut across the migmatitic rocks of the axial zone.
Carte structurale de la partie orientale du dôme gneissique de la Montagne Noire montrant l’orientation et les trajectoires de foliation interprétées (modifiée d’après Rabin et al., 2015). La projection stéréographique montre l’orientation préférentielle des filons de quartz qui recoupent les migmatites de la zone axiale.
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