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Towards fully data driven ground-motion prediction models for Europe
Authors:Boumédiène Derras  Pierre Yves Bard  Fabrice Cotton
Institution:1. Risk Assessment and Management Laboratory (RISAM), Université Abou Bekr Belka?d, Faculté de Technologie. BP 230-13048, Tlemcen, Algerie
2. Institut de Sciences de la Terre (ISTerre), Université Joseph Fourier, CNRS, IFSTTAR, Maison des Géosciences, BP 53, 38041, Grenoble cedex 9, France
3. Institut de Sciences de la Terre (ISTerre), Université Joseph Fourier, CNRS, Maison des Géosciences, BP 53, 38041, Grenoble cedex 9, France
Abstract:We have used the Artificial Neural Network method (ANN) for the derivation of physically sound, easy-to-handle, predictive ground-motion models from a subset of the Reference database for Seismic ground-motion prediction in Europe (RESORCE). Only shallow earthquakes (depth smaller than 25 km) and recordings corresponding to stations with measured $V_{s30}$ properties have been selected. Five input parameters were selected: the moment magnitude $M_{W}$ , the Joyner–Boore distance $R_{JB}$ , the focal mechanism, the hypocentral depth, and the site proxy $V_{S30}$ . A feed-forward ANN type is used, with one 5-neuron hidden layer, and an output layer grouping all the considered ground motion parameters, i.e., peak ground acceleration (PGA), peak ground velocity (PGV) and 5 %-damped pseudo-spectral acceleration (PSA) at 62 periods from 0.01 to 4 s. A procedure similar to the random-effects approach was developed to provide between and within event standard deviations. The total standard deviation ( $\sigma $ ) varies between 0.298 and 0.378 (log $_{10}$ unit) depending on the period, with between-event and within-event variabilities in the range 0.149–0.190 and 0.258–0.327, respectively. Those values prove comparable to those of conventional GMPEs. Despite the absence of any a priori assumption on the functional dependence, our results exhibit a number of physically sound features: magnitude scaling of the distance dependency, near-fault saturation distance increasing with magnitude, amplification on soft soils and even indications for nonlinear effects in softer soils.
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