• Corpus ID: 180259337

IDENTIFYING THE INFLUENCE OF THE LOCAL GEOLOGY IN CASE OF EARTHQUAKE FOR URBAN PLANNING : CASE STUDY IN BRUSSELS

@inproceedings{Rosset2007IDENTIFYINGTI,
  title={IDENTIFYING THE INFLUENCE OF THE LOCAL GEOLOGY IN CASE OF EARTHQUAKE FOR URBAN PLANNING : CASE STUDY IN BRUSSELS},
  author={Philippe Rosset and Toon Petermans and Xavier Devleeschouwer and Franck Pouriel and Thierry Camelbeeck},
  year={2007},
  url={https://api.semanticscholar.org/CorpusID:180259337}
}
It is now widely admitted that the sub-surface geology is a crucial component when analyzing the seismic response in urban areas. Our project aims at mapping the seismic response of a pilot zone of Brussels in case of major earthquake scenarios. A detailed knowledge of spatial underground conditions is essential for an analysis of site effects. This is currently done in Brussels at the scale of 1/5000 through a 2D and 3D GIS model. Geological data, field measurements and numerical modeling… 

Figures from this paper

MAPPING THE LOCAL SEISMIC HAZARD AND ITS INFLUENCE ON BUILT ENVIRONNEMENT : CASE STUDY IN THE MONS BASIN ( HAINAUT-BELGIUM )

Seismic risk is defined as the convolution of the seismic hazard and vulnerability. In the Mons Basin, the conjunction of strong ground motions and the deteriorated state of the built environment

Mapping the local seismic hazard in the urban area of Brussels, Belgium

Several regional earthquakes have been strongly felt and caused damages in and around Brussels during history. For example the magnitude 6-6.5 Verviers earthquake in 1692, which is the strongest

Brussels’ bedrock paleorelief from borehole-controlled power laws linking polarised H/V resonance frequencies and sediment thickness

The empirical power law relation (PR) between resonance frequency (f0), obtained from H/V spectral ratio analysis of ambient noise, and sediment thickness (h), obtained from boreholes, is frequently

Geological and geophysical evidence for large palaeo-earthquakes with surface faulting in the Roer Graben (northwest Europe)

From the analysis of geological, geodetic and geophysical data we provide clear evidence of seismogenic faults capable of producing large earthquakes in intraplate Europe. Previous studies

Large earthquake in northern Europe more likely than once thought

Northern Europe would typically be classified as a relatively stable continental region where seismic hazard is low. Indeed, in comparison to active zones in the Mediterranean, seismic activity is

Use of microtremor measurement for assessing site effects in Northern Belgium – interpretation of the observed intensity during the MS = 5.0 June 11 1938 earthquake

To provide quantitative information on site effects in the northern part of Belgium, forty-seven H/V microtremor measurements were performed with 5 second seismometers over an area of about 15.000