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The Bengal Basin, a significant sediment reservoir at the Ganga-Brahmaputra-Meghna river systems, is shaped by the interaction of the Indian, Eurasian, and Burmese plates, with sediment thickness reaching up to 22 km. The basin features a complex tectonic structure, divided into two major zones, and is influenced by neotectonic activities that have resulted in various geomorphic changes and faulting. Geochronological data indicates the age of basement rocks in the region, with significant geological events

Author

mozammal1997haque

Language

EN