Geological, seismic, and geodynamic studies confirm that the collision of India has far-reaching effects on the geology, crustal deformation, and tectonics of Asian regions well beyond the Himalayas and Tibet.
The retrieved literature consistently supports the claim that the India-Asia collision has broad continental repercussions. Papers [5], [7], and [10] provide explicit evidence of tectonic, seismic, and mantle-flow effects extending into Myanmar, central Tibet, and broader East/Southeast Asia. No papers refute the claim.