(a) Outcrop evidence of overpressure along the Sagaing Fault: sandstones injected into a bedded Miocene sandstone. (a) Outcrop evidence of overpressure along the Sagaing Fault: sandstones injected into a bedded Miocene sandstone. NW suburbs of Naypyidaw. Location: 19.474959° N, 96. 077197° E. (b) Thin-section of sandstone with cataclastic texture with clay matrix, indicating overpressure. R. A. Sloan et al. Geological Society, London, Memoirs 2017;48:19-52 © 2017 The Author(s). Published by The Geological Society of London. All rights reserved