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I.D. Gupta

Researcher at Indian Institute of Technology Roorkee

Publications -  47
Citations -  930

I.D. Gupta is an academic researcher from Indian Institute of Technology Roorkee. The author has contributed to research in topics: Response spectrum & Seismic hazard. The author has an hindex of 15, co-authored 41 publications receiving 779 citations. Previous affiliations of I.D. Gupta include University of Southern California & Central Water and Power Research Station.

Papers
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A Probabilistic Seismic Hazard Analysis of Northeast India

TL;DR: In this article, a new attenuation model for pseudo-spectral velocity scaling has been developed by using 261 recorded accelerograms in Northeast India, and the hazard level has been assessed for each node of this grid by considering the seismicity within a 300-km radius around the node.
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Delineation of probable seismic sources in India and neighbourhood by a comprehensive analysis of seismotectonic characteristics of the region

TL;DR: In this paper, the authors presented a comprehensive description of the various tectonic features and the association of seismicity with them to define the probable seismic sources in India and adjacent areas.
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Order statistics of peaks in earthquake response

TL;DR: In this paper, a probabilistic theory is presented, using order statistics, to find the expected, the most probable, or with any desired confidence level, the amplitudes of all the local maxima in the random response functions at any point in a multistory structure.

The state of the art in seismic hazard analysis

I.D. Gupta
TL;DR: In this paper, a detailed description of both deterministic and probabilistic approaches for seismic hazard analyses is given. But the advantages of using the deterministic approach can simply be achieved via deaggregation of the probablistic hazard analysis.
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Response spectral attenuation relations for in-slab earthquakes in Indo-Burmese subduction zone

TL;DR: In this article, the in-slab earthquakes along the Indo-Burmese subduction zone are found to be characterized by much larger ground motion amplitudes than that for the earthquakes along other subduction zones around the world.