Answers are grounded in this paper and cite their sources.
We present a new approach for performing broad-band ground motion time histories (0.1-30 Hz) of a future earthquake in a sedimentary basin.Synthetics are computed with an hybrid scheme combining reciprocity-based 3-D-spectral element method simulations at low frequencies and empirical Green's functions (EGF) at high frequencies.The combination between both deterministic and empirical parts results in a set of hybrid Green's functions, summed according to a new k -2 kinematic model algorithm.The summation technique enables to remove the high-frequency artefacts that appear above the EGF corner frequency.The ground motion variability is assessed by generating a variety of source parameter sets selected from a priori probability density functions.This leads to a population of response spectra, from which the median spectral acceleration and standard deviation values are derived.The method is applied to simulate a M W 5.5 event in the deep Grenoble basin (French Alps).The comparison with EC8 regulations suggests the need of specific design spectra in the Grenoble valley.
No takes yet. Share an insight, caveat, or question.
Causse et al. (2009) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: