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 …
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 …
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 …
Modelling of 1991 Uttarkashi and 2011 Indo-Nepal earthquakes using the modified semi-empirical technique by integrating site-specific quality factor
Strong ground motion simulation is a reliable tool for seismic hazard assessment and
mitigation of any region. The distribution of hazards during an earthquake is greatly …
mitigation of any region. The distribution of hazards during an earthquake is greatly …
Spatial variability studies of attenuation characteristics of Qα and Qβ in Kumaon and Garhwal region of NW Himalaya
The present work explores the attenuation characteristics of Garhwal and Kumaon regions
of northwest Himalaya, India. A comparative study of P-and S-wave quality factors (Q α and …
of northwest Himalaya, India. A comparative study of P-and S-wave quality factors (Q α and …
Delineation of partial melts and crustal heterogeneities within the crust beneath Kumaon Himalaya, India from Lg wave attenuation
The crustal seismic attenuation or the Q structure is studied by using the Fourier spectra of
Lg-wave along the Tanakpur-Dharchula-Dharma transect in the Kumaon Himalaya. The 1 …
Lg-wave along the Tanakpur-Dharchula-Dharma transect in the Kumaon Himalaya. The 1 …