Summary In Northeast India, three major plates interact along two convergent boundaries:
the Himalayas and the Indo–Burma Ranges, which meet at the Assam Syntaxis. To clarify …

The demarcation of linear geomorphological features due to fracture systems, underlying or
exposed faults, drainage lines etc. from satellite images has been one of the most widely …

An attempt is made to map the spatial variation of the tectonic stress pattern in northeast
India and its adjoining south Asia region using stress tensor inversion of some 516 fault …

Since 1897, ten earthquakes of M≥ 7½ have occurred in north-east India region and its
vicinity including the great earthquakes of June 12, 1897 and August 15, 1950, both of M …

In this study, the crustal shear velocity structure beneath the Indo-Burma Ranges (IBR) is
estimated using inversion modeling of the receiver functions computed at seismic stations …

Abstract The 2016 Mw 6.7 Tamenglong earthquake (in the state of Manipur in northeastern
India) on 4 January 2016 at 04: 35 Indian Standard Time (3 January, 23: 05 UTC) was the …

This study explores the connection between seismic tremors, stress fluctuations, and
structural adjustments in the earth's subsurface. Through b-value calculations, shifts in the …

We studied attenuation of S and coda waves, their frequency and lapse time dependencies
in northeast India in the frequency range of 1–24 Hz. We adopted theories of both single and …

Coda wave attenuation quality factor Qc is estimated in the northeastern region of India
using 45 local earthquakes recorded by regional seismic network. The quality factor Qc was …

Kopili fault has been experiencing higher seismic and tectonic activity during the recent
years. These kind of active tectonics can be inspected by examining coda-wave attenuation …