Deltas, the low-lying land at river mouths, are sensitive to the delicate balance between sea
level rise, land subsidence and sedimentation. Bangladesh and the Ganges-Brahmaputra …

This paper describes geomorphologic evidence for the principal neotectonic features of
Myanmar and its immediate surroundings. We combine this evidence with published …

Earthquakes present severe hazards for people and economies and can be primary drivers
of landscape change yet their impact to river-channel networks remains poorly known. Here …

Abstract The Rakhine (Arakan)‐Bangladesh megathrust, along which the Indian and Burma
plates collide, is assumed by some to be inactive/aseismic due to the lack of notable …

Abstract The Indo-Burmese Arc (IBA) comprises highly populated regions of Northeast India,
Bangladesh, and Myanmar. Thus, quantitative estimation of crustal deformation, earthquake …

Abstract The Indo‐Burma subduction zone is a highly oblique subduction system where the
Indian plate is converging with the Eurasian plate. How strain is partitioned between the …

The active tectonics of the Myanmar (formerly Burma) microplate in central Myanmar are
caused by the oblique collision between the Sunda and Eurasia plates to the east and the …

Abstract The Indo-Burman Ranges (IBR) are an∼ 375 km wide accretionary prism that
accommodates oblique convergence of the∼ 13–20 km thick Ganges–Brahmaputra Delta …

Burma (Myanmar) is situated along the obliquely colliding eastern margin of the Indian Plate
(Fig. 2.1). It connects the ongoing India–Asia collision along the Himalayan Range in the …

Myanmar, one of the most active tectonic regions in the world, endures the risk of destructive
earthquakes. Based on seismic data recorded at the recently deployed dense array of the …