This document is downloaded from DR‑NTU (https://dr.ntu.edu.sg) Nanyang Technological University, Singapore. Geological and tectonic evolution of the Indo‑Myanmar Ranges (IMR) in the Myanmar region Khin, Kyi; Zaw, Khin; Aung, Lin Thu 2017 Khin, K., Zaw, K., & Aung, L. T. (2017). Geological and tectonic evolution of the Indo‑Myanmar Ranges (IMR) in the Myanmar region. Geological Society Memoir, 48(1), 65‑79. doi:10.1144/M48.4 https://hdl.handle.net/10356/144426 https://doi.org/10.1144/M48.4 © 2017 The Author(s). All rights reserved. This paper was published by The Geological Society of London in Geological Society Memoir and is made available with permission of The Author(s). Downloaded on 10 Oct 2021 10:59:28 SGT Geological and tectonic evolution of the Indo-Myanmar Ranges (IMR) in the Myanmar region KYI KHIN1*, KHIN ZAW2 & LIN THU AUNG3 1SK Engineering and Construction, Singapore Branch, 415979, Singapore 2CODES ARC Centre of Excellence in Ore Deposits, University of Tasmania, Private Bag 126, Hobart, Tasmania 7001, Australia 3Earth Observatory of Singapore, Nanyang Technological University, 50 Nanyang Avenue, N2-01a-14, 639798, Singapore *Correspondence:
[email protected] The Indo-Myanmar Ranges (IMR) of Myanmar, also known as of studies in the IMR of Myanmar aiming to understand the the Indo-Burman Ranges (IBR) or the Western Ranges, extend nature and origin of the continental crust beneath Myanmar, from the East Himalayan Syntaxis (EHS) southwards along the significant for Mesozoic and Cenozoic plate tectonic recon- eastern side of the Bay of Bengal to the Andaman Sea, compris- structions of Southeast Asia.