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The Nujiang region along the China-Burma border in the western Yunnan has received a great deal of attention and has been considered to be the important channel of southeastward escape of the Tibetan Plateau[1-4]. This channel is bordered by the Red River-Ailao Mountain left-literal strick-slip fault in the east and Gaoligong- Sagaing right-literal strick-slip fault in the west[5-7]. Within this channel, it is still not clear to which tectonic
The Nujiang region along the China-Burma border in the western Yunnan has a great deal of attention and has been considered to be the important channel of southeastward escape of the Tibetan Plateau. [1-4]. This channel is bordered by the Red River -Ailao Mountain left-literal strick-slip fault in the east and Gaoligong-Sagaing right-literal strick-slip fault in the west [5-7]. Within this channel, it is still not clear to which tectonic