• Laishram Sherjit Singh
• Devesh Walia
• Kh Mohon Singh

Indo Myanmar Range (IMR) is slightly curved and broadly N-S trending fold thrust mountain belt located between the Bengal basin and Central Myanmar basin. It is an active accretionary prism which is composed of Cretaceous ophiolite, Cretaceous to Eocene pelagic sediments, Eocene to Oligocene flysch which is overlain by Neogene shallow water sediments. The complex evolutionary history of IMR is associated with adjoining regions like Bengal basin, Central Myanmar basin and Andaman-Nicobar Island Arc. The Indo-Myanmar-Andaman -Arc evolved through a continental collision during late Oligocene time and followed by the active subduction along the eastern margin of Bengal basin and Andaman trench. Major tectonic and subduction events of IMR have been identified from late Cretaceous to mid- Miocene and Quaternary times. In this paper, we are presenting a brief review of plate boundary, nature of seismicity and seismic vulnerability in IMR

IMR, CMF, subduction, geodynamics, seismicity, vulnerability

"GEODYNAMICS AND SEISMIC VULNERABILITY IN INDO-MYANMAR RANGE", International Journal of Emerging Technologies and Innovative Research (www.jetir.org), ISSN:2349-5162, Vol.5, Issue 8, page no.409-413, August-2018, Available :http://www.jetir.org/papers/JETIRA006074.pdf

"GEODYNAMICS AND SEISMIC VULNERABILITY IN INDO-MYANMAR RANGE", International Journal of Emerging Technologies and Innovative Research (www.jetir.org | UGC and issn Approved), ISSN:2349-5162, Vol.5, Issue 8, page no. pp409-413, August-2018, Available at : http://www.jetir.org/papers/JETIRA006074.pdf