the deformation of quartzites in the Dabie Shan of China is interpreted as coaxial deformation by basal glide (left), non-coaxial deformation by basal glide (center), and coaxial deformation by prism slip (right). Quartz fabeic, Hongan -http://www.geol.ucsb.edu/faculty/hacker/geo102C/lectures/part11.html
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