2018
DOI: 10.1785/0120170184
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Ground‐Motion Simulation by the Empirical Green’s Function Method with a Source Defined by Two Corner Frequencies and a Two‐Stage Summation Scheme

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Cited by 8 publications
(12 citation statements)
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“…In the SSGFM, strong ground motion records for a large-magnitude earthquake (target event) can be defined as a stochastic summation of small-event time histories (EGFs) following a specific source scaling law (Hartzell 1978;Irikura 1983Irikura , 1986Munguia and Brune 1984;Joyner and Boore 1986;Boatwright 1988;Wennerberg 1990;Tumarkin and Archuleta 1994;Ordaz et al 1995;Kohrs-Sansorny et al 2005;Niño et al 2018;. Three steps characterize the stochastic summation process.…”
Section: Methodology For the Stochastic Summation Schemementioning
confidence: 99%
“…In the SSGFM, strong ground motion records for a large-magnitude earthquake (target event) can be defined as a stochastic summation of small-event time histories (EGFs) following a specific source scaling law (Hartzell 1978;Irikura 1983Irikura , 1986Munguia and Brune 1984;Joyner and Boore 1986;Boatwright 1988;Wennerberg 1990;Tumarkin and Archuleta 1994;Ordaz et al 1995;Kohrs-Sansorny et al 2005;Niño et al 2018;. Three steps characterize the stochastic summation process.…”
Section: Methodology For the Stochastic Summation Schemementioning
confidence: 99%
“…These synthetic records were obtained using an improvement of the method originally proposed by Hartzell and modified by Ordaz et al and Kohrs‐Sansorny et al, to enhance the original summation scheme to consider both the uncertainties on the generation process and the parameters which define the physics of the source and dividing it in 2 the summation scheme in two stages. Furthermore, the improved version of the method considers 2 corner frequencies in the definition of the seismic source instead of one as it is usually carried out …”
Section: Determination Of Uniform Fragility Design Spectramentioning
confidence: 99%
“…Furthermore, the improved version of the method considers 2 corner frequencies in the definition of the seismic source instead of one as it is usually carried out. 15 In order to apply the proposed approach at country or region level, it would be necessary to compute, for different sites and seismic sources, the required synthetic accelerograms that collectively represent the seismic hazard that affect the studied region. It is important to point out that it would not be necessary to perform any other further computation among the obtained spectra for different sites, as each one of them will represent the specific seismic demand necessary so that the designed structures to be built in such sites reach the pre-established target performance.…”
Section: Seismic Simulationmentioning
confidence: 99%
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