Figure 1a). Oblique-subduction of the Indian Plate beneath the West Burma Block, southeastern Tibetan Plateau uplifting, formation of the EHS, crustal lateral extrusion and clockwise rotation, and tectonic evolution of strike-slip fault systems are major Cenozoic tectonic events of Southeast Asia. The coherent compression between the Indian Plate and Eurasia was suggested to provide the driving force for significant crustal clockwise rotational extrusion from the southeastern Tibetan Plateau, which controlled the Cenozoic tectonic evolution of strike-slip faults systems in