Physics
Scientific paper
May 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30i...6c&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 9, pp. 6-1, CiteID 1453, DOI 10.1029/2002GL016593
Physics
2
Seismology: Earthquake Ground Motions And Engineering, Seismology: Seismic Hazard Assessment And Prediction, Seismology: Instruments And Techniques
Scientific paper
We study multi-dimensional site effects in the small-size deep sediment filled basin of Grenoble (French Alps). A very dense array composed of 3-component seismometers over a 1 km aperture is used to investigate propagation parameters of waves propagating across the array. We present results for 6 teleseismic events for which we had a reference rock site. For the frequency range 0.1 to 1 Hz, records are clearly dominated by edge-generated surface waves. Quantification of energy carried by each identified wave train allows interpreting the difference between site-to-bedrock and 1D transfer function estimates in terms of laterally propagating basin-edge induced waves only above the fundamental resonance frequency of the basin. A simple ratio between site-to-bedrock and 1D transfer function curves should thus provide an estimation of the relative contribution of 1D and 2D/3D effects in ground motion on the condition that all the time signal length is taken into account.
Bard Pierre-Yves
Cornou Cécile
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