Seismic landslide hazard assessment of central seismic gap region of Himalaya for a Mw 8.5 scenario event
In this study, seismic landslide hazard analysis is performed for central seismic gap (CSG)
region of Himalaya for a future scenario earthquake of magnitude (M w) 8.5. Initially, PGA …
region of Himalaya for a future scenario earthquake of magnitude (M w) 8.5. Initially, PGA …
A simplified method for simulation of strong ground motion using finite rupture model of the earthquake source
A Joshi, S Midorikawa - Journal of seismology, 2004 - Springer
We present a simplified method to simulate strong ground motion for a realistic
representation of a finite earthquake source burried in a layered earth. This method is based …
representation of a finite earthquake source burried in a layered earth. This method is based …
The simulation of ground motions using envelope summations
The technique of Midorikawa (1993) has been modified to obtain a resultant envelope
function at the observation point by placing the rupture causing an earthquake in a layered …
function at the observation point by placing the rupture causing an earthquake in a layered …
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 …
Simulation of strong ground motion due to active Sohna fault in Delhi, National Capital Region (NCR) of India: an implication for imminent plausible seismic hazard
Abstract Delhi, National Capital Region (NCR) of India, falls in the seismic Zone IV (Zone
factor 0.24) on the seismic zoning map prepared by the Bureau of Indian Standards (BIS) …
factor 0.24) on the seismic zoning map prepared by the Bureau of Indian Standards (BIS) …
Aftershock activity and frequency-dependent low coda Qc in the epicentral region of the 1999 Chamoli earthquake of Mw 6.4
On 28 March, 1999 (19: 05: 10.09, UT) a significant earthquake of M w 6.4 occurred in the
Garhwal Himalaya (30.555° N, 79.424° E). One hundred and ten well-recorded aftershocks …
Garhwal Himalaya (30.555° N, 79.424° E). One hundred and ten well-recorded aftershocks …
Emergence of the semi-empirical technique of strong ground motion simulation: A review
High frequency ground motion simulation techniques are powerful tools for designing
earthquake resistant structures in seismically active regimes. Simulation techniques also …
earthquake resistant structures in seismically active regimes. Simulation techniques also …
Simulation of strong ground motions of 1991 Uttarkashi (M 7) and 1999 Chamoli (M 6.6) earthquakes using modified hybrid technique
In the present study, 1991 Uttarkashi (M 7) and 1999 Chamoli (M 6.6) earthquakes that
occurred on October 19, 1991, at 21: 23: 14 h and March 28, 1999, at 19: 05: 11 h …
occurred on October 19, 1991, at 21: 23: 14 h and March 28, 1999, at 19: 05: 11 h …
Estimation of strong ground motion from a great earthquake Mw 8.5 in central seismic gap region, Himalaya (India) using empirical Green's function technique
In the present study ground motions for a Mw 8.5 scenario earthquake are estimated at 13
sites in Kumaun-Garhwal region using the empirical Green's function technique. The …
sites in Kumaun-Garhwal region using the empirical Green's function technique. The …
Evaluating the seismic hazard to Sikkim region of Himalaya using simulated accelerograms
R Yadav, D Kumar - Journal of Earth System Science, 2022 - Springer
Abstract The 2011 Sikkim earthquake (M 6.9) of the Himalaya has shown that a moderate
size earthquake may also cause severe damage to the region. Simulated accelerograms …
size earthquake may also cause severe damage to the region. Simulated accelerograms …