Probabilistic seismic hazard assessment for northeast India region
Northeast India bounded by latitudes 20°–30° N and longitudes 87°–98° E is one of the
most seismically active areas in the world. This region has experienced several moderate-to …
most seismically active areas in the world. This region has experienced several moderate-to …
Obtaining the surface PGA from site response analyses based on globally recorded ground motions and matching with the codal values
Destructive moderate to major earthquakes across the globe have highlighted various
possible forms and extent of damages. Subsoil properties play a vital role in controlling the …
possible forms and extent of damages. Subsoil properties play a vital role in controlling the …
Spatial distribution of bedrock level peak ground acceleration in the National Capital Region of India using geographic information system
The probabilistic seismic hazard analysis is conducted for the seismically active National
Capital Region (NCR) of India, one of the most densely populated regions in the world, to …
Capital Region (NCR) of India, one of the most densely populated regions in the world, to …
Comprehensive amplification estimation of the Indo Gangetic Basin deep soil sites in the seismically active area
K Bajaj, P Anbazhagan - Soil Dynamics and Earthquake Engineering, 2019 - Elsevier
Site amplification coefficients and acceleration design response spectra (ADRS) for the
deep Indo-Gangetic Basin (IGB) have been proposed. Non-linear site response analysis is …
deep Indo-Gangetic Basin (IGB) have been proposed. Non-linear site response analysis is …
Micro-seismic hazard assessment of Ahmedabad city, Gujarat (Western India) through near-surface characterization/soil modeling
K Mohan, S Dugar, V Pancholi, V Dwivedi… - Bulletin of Earthquake …, 2021 - Springer
The micro-seismic hazard estimation including quantification of the ground motion
amplification has been conducted at Ahmedabad city based on near-surface …
amplification has been conducted at Ahmedabad city based on near-surface …
Tectonic geomorphology along the transverse basement fault (Moradabad fault) in the Ganga basin: A nexus between the Himalayan tectonics and the pre-Himalayan …
The present study focuses on the neotectonic perspective of a subsurface basement fault, ie,
the Moradabad Fault (MF) in the Ganga basin. This is a∼ 163 km long NE-SW trending …
the Moradabad Fault (MF) in the Ganga basin. This is a∼ 163 km long NE-SW trending …
Probabilistic seismic hazard mapping of National Capital Region of India using a modified gridded seismicity model
A Gupta, ID Gupta, VK Gupta - Soil Dynamics and Earthquake Engineering, 2021 - Elsevier
This is the first comprehensive study for a seismic macro-zonation of the National Capital
Region of India by using the probabilistic seismic hazard analysis approach. A modified …
Region of India by using the probabilistic seismic hazard analysis approach. A modified …
Determination of NEHRP site class of seismic recording stations in the Northwest Himalayas and its adjoining area using HVSR method
NH Harinarayan, A Kumar - Pure and Applied Geophysics, 2018 - Springer
Local site characteristics play an important role in controlling the damage pattern during
earthquakes (EQs). These site characteristics may vary from simple to complex and can be …
earthquakes (EQs). These site characteristics may vary from simple to complex and can be …
Recent seismicity in Delhi and population exposure to seismic hazard
S Kolathayar - Natural Hazards, 2021 - Springer
This paper makes an attempt to review historical and recent seismicity in Delhi and presents
updated seismic hazard map of Delhi integrated with ward-wise classified population data …
updated seismic hazard map of Delhi integrated with ward-wise classified population data …
Long period ground motion at bedrock level in Delhi city from Himalayan earthquake scenarios
Delhi, the capital of India, is prone to severe seismic hazards, not only from local events but
also from Himalayan earthquakes at distances of 250–300 km. Standard techniques are not …
also from Himalayan earthquakes at distances of 250–300 km. Standard techniques are not …