Supplemental Material: Southeastward migration of the Eastern Himalayan Syntaxis since the late Miocene: New insights from crustal rotational deformation of the Tengchong Terrane on the southeastern margin of the Tibetan Plateau

Key Points

• The research shows substantial southeastward movement of the Eastern Himalayan Syntaxis since the late Miocene.
• Paleomagnetic results from volcanic rocks in the Tengchong Terrane indicate substantial geological shifts and rotations.
• Assessment of crustal rotational deformation reveals insights into tectonic processes affecting the Tibetan Plateau.
• These findings suggest a dynamic geological history for the region, highlighting migration patterns and crustal behaviors.