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In the present paper, we describe ductile and brittle deformation styles in western Yunnan and NE Myanmar, using field data and Landsat 7 imagery. We show that this complex area located at the northern termination of Sunda Plate (Three Rivers area) was wedged during the Tertiary between the left-lateral Ailao Shan/Chong Shan metamorphic belts to the east and the right-lateral Shan scarp/Gaoligong...
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