... Sunda Arc, which includes the Indo-Burmese wedge (IBW) in the forearc and the Sagaing fault in the backarc, are very poorly constrained. Plate reconstruction models and geological structures in the region suggest that subduction in the IBW occurred in the geological past, but whether it is still active...

.... This fold belt of the Bengal Basin along with more easterly Indo-Burman Range (IBR) developed as a consequence of the oblique collision between Indian and Burmese plates. This neotectonic activity is still continuing and shaping the geomorphology of the area. This study is conducted based...

...Ananya Biswas; Bhabani Prasad Mukhopadhyay Abstract Geological domains in northeastern India evolved though time after the rupture of the Gondwanaland. Collision of the Indian and the Burmese plates took place during the middle part of Cretaceous. Evolution of the Paleogene Barail trough, Neogene...

...A. P. Singh; N. Purnachandra Rao; M. Ravi Kumar; M.‐C. Hsieh; L. Zhao Abstract The Burmese arc is a peculiar plate boundary where there exists an eastward subducted Indian slab, but the current tectonics of the region are predominantly governed by a northward strike‐slip motion of the Indian plate...

... times, due to interaction of the Indian, Tibetan, and Burmese plates. The high seismicity indicates that the movements are continuing. The seismic zone underlying Burma is approximately V shaped and dips toward the east underneath Arakan-Yoma. Most of the intermediate-focus earthquakes in Burma underlie...

...S. V. Desikachar Abstract The distinctive characteristics and independent evolution until Neogene times of the Bengal basin situated on the Indian plate and the Assam-Arakan basin situated on the Burmese plate, are described. The Indian plate during this period was simultaneously in the process...

...B. P. Duarah; Sarat Phukan Abstract Shillong Plateau in India is tectonically and geologically interesting entity in the subducted front of Indian Plate below Burmese Plate to the southeast and Tibetan Plate to the north and associated with thrusts and shears along the plate boundaries. Horse-tail...

... tectonics of the region: collision of the Indian plate with the Eurasian plate at the Himalaya and subduction of the Indian plate beneath the Burmese plate at the Arakan-Yoma range . 08 1 1986 Copyright © 1987, by the Seismological Society of America References...

... of the Indian Plate beneath the Eurasian and Burmese Plates. The Hatia Trough is a proven petroleum province that occupies much of the southern Bengal Basin. However, the style of deformation, kinematics, and possible timing of structural initiation in the Hatia Trough and the relationship of this deformation...

... to convergence of Indian plate with Burmese plate. Structures of the shallower and deeper reflectors are formed at different phases of structural development. Seismic sections and well logs of the Titas structure were collected from the BAPEX data centre located at the head office of BOGMC (Petrobangla...

...A. Serpetsidaki; N. K. Verma; G.‐A. Tselentis; N. Martakis; K. Polychronopoulou; P. Petrou Abstract Northeast India has been subjected to extensive compressional forces, mainly in north–south and east–west directions resulting from the convergence of the Indian plate with the Eurasian and Burmese...

...Md. Sakawat Hossain; Songjian Ao; Tridib Kumar Mondal; Arnab Sain; Md. Sharif Hossain Khan; Wenjiao Xiao; Pengpeng Zhang Abstract The tectonic deformation of the outer Indo-Burman Ranges (i.e., Chittagong Tripura Fold Belt, CTFB) is associated with the oblique convergence of Indo-Burmese plates...

... and oceanic arc setting developed in the Neo-Tethys oceanic domain between the Indian and Burmese plates during the Late Cretaceous. © 2021 The Author(s). Permission for reuse (free in most cases) can be obtained from copyright.com . 24 9 2020 4 3 2021 Published by NRC Research Press...

...Fig.2. Schematic interplate configuration below NBA (approach adopted after Sibson, 2009 ); BP: Burmese Plate, CSZ – Crustal Seismic Zone; within CSZ of Burma plate seismicity is sparse in the forearc domain below CB – Chindwin Basin while large earthquakes occur in the backarc domain associated...

... factors, including oblique subduction, arc volcanism, and the ill-defined Andaman spreading ridge in the Andaman Sea. The oceanic lithosphere of the Indian plate subducts eastward below the oceanic part of the Burmese plate in southeast Asia ( Curray et al. , 1979 ) identified by the Andaman–Sumatra...

..., and between Indian and Burmese plates in the NE resulting in Assam-Arakan fold and fold-thrust belt. Both these collisions occurred during early Cenozoic and have produced large swath of foreland sedimentary basins, which produced fold-thrust belts (FTB) during Neogene due to continued convergence...

..., and of the active margin on the Burma Terrane, where the Indian plate subducts below the western edge of peninsular Indochina ( Fig. 1A ), remain virtually undocumented and are the focus of intense speculation. Reconstructing the history of the Burmese margin is, however, a prerequisite for any paleotectonic...

... late Jurassic to early Cretaceous is directly related with the break-up of eastern Gondwanaland and collision of the Indian plate with the Asian plate to the north and Burmese plate to the east. The Eastern Fold Belt (EFB) or Chittagong Tripura Fold Belt (CTFB) is considered to be the youngest...

...Abhijit Deonath; Basab Mukhopadhyay Abstract The western margin of Sundaland is affected by two major tectonic events, the India-Eurasia collision and subduction along the Burmese-Andaman-Sunda Arc. Geotectonic analysis of the Burmese-Andaman-Sunda Arc areas reveals that it represents an arc...