2020
DOI: 10.1007/s11069-020-04068-8
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Ground motion modelling in northwestern Himalaya using stochastic finite-fault method

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Cited by 8 publications
(4 citation statements)
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“…Seismic hazard map has been developed for 0.025 o ×0.025 o size grid and it has been observed that PGA SUR values lies between 0.140 to 0.280 g. It has also been observed that higher PGA values for the region lies in proximity to Lineament 2. For better estimation of seismic hazard in the NW Himalaya region [30], also conducted the studies related to PGA estimation in the region using stochastic approach and calculated values of PGA at 2346 locations covering an area of about 1000000 km 2 of NW Himalaya and provided a PGA map of the study area with extreme resolution of 0.2 degree for better estimate of seismic danger in the region. Higher surface PGA SUR values (> 0.27 g) have been found for the middle portion of the study area including sites GRL-10, 11, 12 and 17 along with higher depth of GWT.…”
Section: Resultsmentioning
confidence: 99%
“…Seismic hazard map has been developed for 0.025 o ×0.025 o size grid and it has been observed that PGA SUR values lies between 0.140 to 0.280 g. It has also been observed that higher PGA values for the region lies in proximity to Lineament 2. For better estimation of seismic hazard in the NW Himalaya region [30], also conducted the studies related to PGA estimation in the region using stochastic approach and calculated values of PGA at 2346 locations covering an area of about 1000000 km 2 of NW Himalaya and provided a PGA map of the study area with extreme resolution of 0.2 degree for better estimate of seismic danger in the region. Higher surface PGA SUR values (> 0.27 g) have been found for the middle portion of the study area including sites GRL-10, 11, 12 and 17 along with higher depth of GWT.…”
Section: Resultsmentioning
confidence: 99%
“…6.1 Strong Ground Motion and Earthquake Hazard Assessment 6.1.1 Plate boundary regions Mir and Parvez (2020) simulated bedrock level peak ground motion at 2346 sites on a regular grid of 0.2 • x0.2 • in NW Himalaya from 543 simulated sources, using the stochastic finite-fault, dynamic corner frequency method, with particular emphasis on Kashmir Himalaya. Acceleration time series generated are then integrated to obtain velocity and displacement time series, which are all used to construct a suite of hazard maps of the region.…”
Section: Seismic Hazard Risk and Strong Ground Motion Studiesmentioning
confidence: 99%
“…In general, there are two types of ground motion-the real ground-motion records obtained by seismic stations in the advent of earthquakes, and synthetic ground motion. Real ground motions are obtained from the ground-motion database [1], whereas several methodologies are employed to obtain synthetic ground motions [2,3]. Many factors affect the structural response (e.g., load uncertainty, structural material, and construction quality), among which load uncertainty has the highest influence [4,5], and ground-motion input (as an important part of the structural load input) has a considerable effect.…”
Section: Introductionmentioning
confidence: 99%
“…Ground-motion-synthesis methodologies have been developed for many years, and several researchers have proposed different methods to simulate ground motions based on different principles. Currently, ground-motion-simulation methods are divided into three categories: (1) Ground-motion simulation based on the stochastic method; (2) physicsbased ground-motion-simulation methods; and (3) hybrid simulated ground motions [3,[7][8][9][10][11]. Numerous techniques for simulating ground motion are currently under investigation [12][13][14][15][16][17].…”
Section: Introductionmentioning
confidence: 99%