Titlebook: Best Practices in Physics-based Fault Rupture Models for Seismic Hazard Assessment of Nuclear Instal; Luis A. Dalguer,Yoshimitsu Fukushima

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,Dynamic Rupture Modelling of the 1999 Düzce, Turkey Earthquake,he deep, middle and shallow) and strong barriers between asperities. S. is as high as 19 Mpa at barriers between the three asperities and ∆τ is maximum about 40 Mpa at the deepest asperity. This heterogeneity in stress distribution produces abrupt jumps in rupture velocity, exhibiting locally appare

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Accommodation

Quantification of Fault-Zone Plasticity Effects with Spontaneous Rupture Simulations,s than 1% in massive, high-quality rock. These reductions are almost insensitive to magnitude. If the stress drop is doubled, plasticity reduces near-fault PGVs by 38–45% and 5–15% in rocks of low and high strength, respectively. Because non-linearity reduces slip rates and static slip near the surf

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Within-Event and Between-Events Ground Motion Variability from Earthquake Rupture Scenarios,event and between-events ground motion variability increase when the slip correlation length on the fault increases. The probability density functions of ground motion tend to truncate at a finite value when the correlation length of slip decreases on the fault, therefore, we do not observe any long

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Azimuthal Dependence of the Ground Motion Variability from Scenario Modeling of the 2014 Mw6.0 Soutrface, avoiding unrealistically strong ground motions. Rupture velocity can also have random variations, which result in irregular rupture front while satisfying the causality principle. This advanced kinematic broadband source model is freely available and can be easily incorporated into any numeri

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,Near-Fault Broadband Ground Motion Simulations Using Empirical Green’s Functions: Application to thn Upper Rhine Graben (URG), at the French–German border. URG is a region where faults producing micro-seismic activity are very close to the sites of interest (e.g., critical infrastructures like supply lines, nuclear power plants, etc.) needing a careful investigation of seismic hazard. In this wor

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