1. (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: ° N, ° 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