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Re-estimation of the location and size of the pre-instrumented 1 September 1803 Garhwal–Kumaon Himalaya earthquake: evidence from site characterization and …
Abstract The historical 1 September 1803 Garhwal–Kumaon Himalaya earthquake (Mw 8.1)
was a solitary Himalayan earthquake reported felt widely in the Indo-Gangetic Plain with …
was a solitary Himalayan earthquake reported felt widely in the Indo-Gangetic Plain with …
3D attenuation tomography of the Uttarakhand, NW Himalaya: Linkage to fluid or partial melt Zones-seismic hazard
This work proposes the shear-wave attenuation tomography of the Garhwal and Kumaun
regions, Uttarakhand Himalaya, to investigate the crustal state. Based on attenuation …
regions, Uttarakhand Himalaya, to investigate the crustal state. Based on attenuation …
Testing the performance of earthquake early warning system in northern India
The main goal of present study is to test the functionality of an earthquake early warning
(EEW) system (a life-saving tool), in India using synthesized data and recorded earthquake …
(EEW) system (a life-saving tool), in India using synthesized data and recorded earthquake …
Development of region specific earthquake early warning scaling relations for the Garhwal region using observed and simulated datasets: a step forward to disaster …
The Garhwal region, situated in the central segment of the Himalayas, stands as one of the
most seismically active areas in the Uttarakhand Himalaya. The newly established …
most seismically active areas in the Uttarakhand Himalaya. The newly established …
Insights into the crustal heterogeneity of Bhutan Himalaya from high frequency body wave attenuation characteristics
In this study, we aim to understand the characteristics of the crust beneath Bhutan Himalaya
in terms of body wave attenuation properties. Extended coda normalization method …
in terms of body wave attenuation properties. Extended coda normalization method …
Modeling of strong ground motions for 1991 Uttarkashi, 1999 Chamoli earthquakes, and a hypothetical great earthquake in Garhwal–Kumaun Himalaya
In this study, stochastic finite fault modeling is used to simulate Uttarkashi (1991) and
Chamoli (1999) earthquakes using all available source, path, and site parameters available …
Chamoli (1999) earthquakes using all available source, path, and site parameters available …
Detailed Attenuation Study of Shear Waves in the Kumaon Himalaya, India, Using the Inversion of Strong‐Motion Data
The frequency‐dependent shear‐wave quality factor Q β (f) of the seismically active Kumaon
Himalaya was calculated using strong‐motion data recorded between 2006 and 2012. The …
Himalaya was calculated using strong‐motion data recorded between 2006 and 2012. The …
Attenuation character of seismic waves in Sikkim Himalaya
In this study, we investigate the seismic wave attenuation beneath Sikkim Himalaya using P,
S and coda waves from 68 local earthquakes registered by eight broad-band stations of the …
S and coda waves from 68 local earthquakes registered by eight broad-band stations of the …
The Attenuation of High‐Frequency Seismic Waves in the Lower Siang Region of Arunachal Himalaya: Qα, Qβ, Qc, Qi, and Qs
In the present study, the scattering and intrinsic attenuation are separated using the S‐wave
attenuation (Q β) and coda‐wave attenuation (Q c) employing the method, and the …
attenuation (Q β) and coda‐wave attenuation (Q c) employing the method, and the …
Regional variation of coda Q in Kopili fault zone of northeast India and its implications
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 …
years. These kind of active tectonics can be inspected by examining coda-wave attenuation …