Intensity Assessment and Seismotectonic Causes of Historical Earthquakes in Bangladesh and Surrounding Areas
DOI:
https://doi.org/10.64862/Keywords:
Earthquake Catalog, Declustering, Gutenberg-Richter Relationship, b-value, Peak Ground AccelerationAbstract
Bangladesh lies at the junction of the Indian and Eurasian plates with the Burmese sub-plates, one of the most seismically active regions of South Asia, yet existing hazard models are largely outdated. A declustered and completeness-screened earthquake catalog has been compiled for Bangladesh and its surrounding tectonic setting, removing 46.5% of the original catalog as dependent aftershocks and foreshocks and leaving 2,811 independent events. The Gutenberg–Richter recurrence analysis, limited to earthquakes of Mw ≥ 4.5, gave a b-value of 0.97 — within the range typical of ordinary crustal seismicity — and a mean return period of ~437 years for a Mw 8.0 event, close to the ~400-year strain-accumulation cycle estimated from GPS geodesy. Mapping earthquake density reveals three concentrated zones: the Sylhet–northeastern border, the Chittagong Hill Tracts, and a cluster along the Madhupur Fault just north of Dhaka. Each zone is independently supported by Peak Ground Acceleration (PGA) values from a global hazard model, ranging from 0.14g–0.2g near Dhaka to 0.26g–0.29g in the Chittagong Hill Tracts. These results suggest an underrecognized intraplate fault north of the capital shapes seismic hazard as much as the country's two major plate-boundary systems — the Shillong Plateau margin and the Indo-Burman subduction zone.
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