Indo-Myanmar (Burma) Ranges (IMR) have a distinct entity in the tectonic framework of Eastern Himalaya and the Southeast Asia. The IMR, which is thought to be northern prolongation of the Indonesian island are linking with the Himalaya possibly along the Tidding Suture Zone, is believed to have evolved due to subduction of the Indian plate below the Myanmar (Burma) plate. In the process, the range evolved as an accretionary prism of imbricate thrust system where ...
