Fig. 13
From: The structural history of the Mont Blanc massif with regard to models for its recent exhumation
Gradient in Alpine deformation within the Mont Blanc shear zone. a Strongly sheared granite close to the basement-cover contact at Col de Balme [563843/097237]. b Folded aplitic dyke and strong Alpine fabric ~400 m SE of the Plan de l’Aiguille cable-car station [557308/083104]. c Preserved pre-Alpine structures cut by aplitic dykes unaffected by Alpine deformation ~600 m SW of the Plan de l’Aiguille cable-car station [557363/082891]. One euro piece for scale