Interpretation cinematique des deformations plastiques dans le massif de Lherzolite de lanzo (Alpes piemontaises) — comparaison avec d'autres Massifs

A map of internal movements into the Lherzolite Massif of Lanzo (shear planes, movement directions, shear senses, estimation of movements intensity) has been drawn from systematic measurements of plastic deformation elements (foliation planes, enstatite lineations, shear senses and angles, grain size of the rocks) which have been taken both in the field and laboratory. Since the deformation is probably due to the intrusion of the massif, these results contribute to knowledge of the orogenic displacements in this area of the Alpine system.