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Seismic zonation of Nepal using probabilistic seismic hazard analysis

Arabian Journal of Geosciences, 2021
Probabilistic seismic hazard of Nepal (PSHA) followed by seismic zonation is carried out for enclosed polygon within 26.5°N–30.5°N latitude and 80°E–89°E longitude. Mixed type of ground motion prediction equations (GMPEs) derived for active shallow crustal and subduction interference with areal and linear sources was used by logic tree approach.
Hari Ram Parajuli   +2 more
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Sequence-Based Probabilistic Seismic Hazard Analysis

Bulletin of the Seismological Society of America, 2014
Abstract Earthquakes are typically clustered both in space and time. Only mainshocks, the largest magnitude events within each cluster, are considered by classical seismic hazard, which is expressed in terms of rate of exceedance of a ground‐motion intensity measure at a site of interest (Cornell, 1968).
IERVOLINO, IUNIO   +2 more
openaire   +3 more sources

On Multisite Probabilistic Seismic Hazard Analysis

Bulletin of the Seismological Society of America, 2016
Abstract Seismic hazard assessment, in its classical format, models the stochastic process of occurrence of earthquakes causing the exceedance of ground‐motion intensity measure (IM) thresholds at a specific site. This is because civil structures typically require probabilistic seismic hazard analysis (PSHA) for one location.
Giorgio, Massimiliano, IERVOLINO, IUNIO
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Probabilistic seismic hazard analysis in Nepal

Earthquake Engineering and Engineering Vibration, 2013
The seismic ground motion hazard for Nepal has been estimated using a probabilistic approach. A catalogue of earthquakes has been compiled for Nepal and the surrounding region (latitude 26° N and 31.7° N and longitude 79° E and 90° E) from 1255 to 2011.
Thapa Dilli Ram, Guoxin Wang
openaire   +1 more source

Probabilistic Seismic Hazard Analysis for Induced Seismicity

2014
Probabilistic Seismic Hazard Analysis is currently the most common approach to seismic hazard analysis. For application to induced seismicity, a major challenge is the fact that the hazard is inherently nonstationary. In this paper we describe the theoretical extension of PSHA to a non-stationary context.
Kraaijpoel D A   +3 more
openaire   +2 more sources

Problems for Probabilistic Seismic Hazard Analysis

Natural Hazards, 1997
The use of b-values derived from the Gutenberg–Richter relationship as a phenomenological base for developing probabilistic seismic hazard analyses (PSHA) has been questioned for years. The relationship is still used because political demands require something for PSHA, one variable is easy to deal with, and no persuasive alternative has come forward ...
D. H. Speidel, P. H. Mattson
openaire   +1 more source

Probabilistic Seismic Hazard Analysis Code Verification

PEER Reports, 2018
Over the past decade, the use of Probabilistic Seismic Hazard Analysis (PSHA) to assess seismic hazards has expanded, leading to the creation of a number of new PSHA computer codes throughout the industry. Additionally, recent seismic source and ground-motion characterization studies have led to more complex source and ground-motion models, which ...
Christie Hale   +2 more
openaire   +1 more source

Probabilistic seismic hazard analysis for Bangalore

Natural Hazards, 2008
This article presents the results of probabilistic seismic hazard analysis (PSHA) for Bangalore, South India. Analyses have been carried out considering the seismotectonic parameters of the region covering a radius of 350 km keeping Bangalore as the center. Seismic hazard parameter ‘b’ has been evaluated considering the available earthquake data using (
Anbazhagan, P, Vinod, JS, Sitharam, TG
openaire   +1 more source

A Unified Probabilistic Framework for Seismic Hazard Analysis

Bulletin of the Seismological Society of America, 2017
The proper scientific interpretation of the seismic hazard estimates requires a probabilistic framework that admits epistemic uncertainties on aleatory variables. This is not straightforward because, to subjectivists, all probabilities are epistemic, whereas to frequentists, all probabilities are aleatory.We illustrate the inadequacy of purely ...
Marzocchi, W., Jordan, T. H.
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Probabilistic seismic hazard analysis for seismic sequences

2013
Earthquakes are typically clustered both in space and time. Seismic h azard , expressed in terms of rate of exceedance of a ground motion intensity measure , classically refers to ma i nshock s, which means that such a rate is computed filtering the rate o f occurrence of events of largest magnitude within each cluster of earthquakes.
IERVOLINO, IUNIO   +2 more
openaire   +3 more sources

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