Abstract:In this peper, by stodyting the geometry, dynamics and kinematics of the tectonic lenses in the midde part of the Yishu fault zone, the author points out that the lenses are commonly distributed symetrically and in zonation,The sehistosity zone is the result of further compression and grinding. According to the Lenses asymmetrical distribution pattern and their relationship with the adjacent fault, the author can determine the mechanical property and the sense of movement of the fault. It is concluded that...