Fig. 7From: The Maira-Sampeyre and Val Grana Allochthons (south Western Alps): review and new data on the tectonometamorphic evolution of the Briançonnais distal marginOrientation of the structural elements in the studied area. Stereoplots (Wulff net, lower hemisphere) simplified after Henry et al., 1993 (a, b), Horrenberger & Michard, 1978 (c, f), Schumacher, 1972 (d, e) and Lefèvre and Michard, 1976 (g, h). In g, the black dots mainly correspond to S3 fanned cleavage, but possibly also to the folded S2 foliationBack to article page