Deepwater fold and thrust belts (DWFTBs) are classified into near-field stress-driven Type 1 systems confined to the sedimentary section, and Type 2 systems deformed by either far …
MS Steckler, SH Akhter, L Seeber - Earth and Planetary Science Letters, 2008 - Elsevier
We take a fresh look at the topography, structure and seismicity of the Ganges–Brahmaputra Delta (GBD)–Burma Arc collision zone in order to reevaluate the nature of the accretionary …
T Maurin, C Rangin - Tectonics, 2009 - Wiley Online Library
The northern Sunda subduction zone, offshore Burma, and the associated Indo‐Burmese Wedge mark the active eastern boundary of the Burma Platelet jammed between the India …
MS Hossain, MSH Khan, KR Chowdhury… - Tectonics and structural …, 2019 - Springer
Abstract The Bengal Basin is a collisional foreland basin in South Asia located at the juncture of the Eurasian, Indian and Burmese Plates occupying Bangladesh and parts of the …
MA Islam - Journal of Asian Earth Sciences, 2009 - Elsevier
This study deals with the diagenesis and reservoir quality of sandstones of the Bhuban Formation located at the Titas Gas Field of Bengal Basin. Petrographic study including XRD …
Large-scale geological sequestration of CO2 is one of the most effective strategies to limit global warming to below 2° C, as recommended by the Intergovernmental Panel on Climate …
Subduction complexes large enough to be exposed subaerially and become significant sources of terrigenous detritus are formed by tectonic accretion above trenches choked with …
The Cenozoic sedimentary succession of Bangladesh provides an archive of Himalayan erosion. However, its potential as an archive is currently hampered by a poor …
A clear insight of the Indo-Burma amalgamation is required for an understanding of the complex processes of the Indo-Asian collision. Where and when the northeastern part of the …