Seismicity in the vicinity of the India-Burma border: Evidence for a sinking lithosphere

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Abstract

The vicinity of the India-Burma border region is among a few intracontinental regions in the world where intermediate-focus earthquakes occur. The recent installation of new seismic stations has improved the detection and location capabilities for earthquakes in this region. Three seismic stations belonging to this new array are located over the zone of intermediate-focus earthquakes. Analysis of recently acquired seismic data reveals a well-defined near-vertical zone of earthquake foci extending to 200 km beneath the Arakan-Yoma fold belt. On the basis of seismic, gravity and other geological data, it is suggested that this zone of earthquakes is associated with remnants of the already subducted, but not totally assimilated, Tethys oceanic lithosphere below the Burmese plate. © 1986.

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Gupta, H. K., & Bhatia, S. C. (1986). Seismicity in the vicinity of the India-Burma border: Evidence for a sinking lithosphere. Journal of Geodynamics, 5(3–4), 375–381. https://doi.org/10.1016/0264-3707(86)90016-5

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