2019
DOI: 10.1029/2019gl083438
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Train Traffic as a Powerful Noise Source for Monitoring Active Faults With Seismic Interferometry

Abstract: Laboratory experiments report that detectable seismic velocity changes should occur in the vicinity of fault zones prior to earthquakes. However, operating permanent active seismic sources to monitor natural faults at seismogenic depth is found to be nearly impossible to achieve. We show that seismic noise generated by vehicle traffic, and especially heavy freight trains, can be turned into a powerful repetitive seismic source to continuously probe the Earth's crust at a few kilometers depth. Results of an exp… Show more

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Cited by 94 publications
(97 citation statements)
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“…Seismic data recorded during the lockdown might be particularly useful in identifying sources of anthropic noise, which could be employed by geophysicists, after the lockdown, e.g. to characterise the upper subsoil by cross correlation of ambient signal 23,24 .…”
Section: The Spectral Signature Of "Cultural" Seismic Noisementioning
confidence: 99%
“…Seismic data recorded during the lockdown might be particularly useful in identifying sources of anthropic noise, which could be employed by geophysicists, after the lockdown, e.g. to characterise the upper subsoil by cross correlation of ambient signal 23,24 .…”
Section: The Spectral Signature Of "Cultural" Seismic Noisementioning
confidence: 99%
“…Previous studies revealed that the noise generated by human infrastructures can be clearly observed at distances larger than 10 km, nevertheless subsurface properties may significantly impact on the distance over which noise propagates 16 , 17 . Since the average interstation distance is around 32 km (figure S2 ), values at specific sites are indeed representative of the average noise level in a broader area around the observation point, especially where the density of stations is higher and the characteristics of noise are similar.…”
Section: Discussionmentioning
confidence: 99%
“…Furthermore, recently, it has become possible to use these anthropogenic noises for the visualization of near-surface structures since the recent development of permanent high-quality seismic networks and the development of techniques. Anthropogenic seismic noises, such as tra c and trains, were used to extract shear, compressional, or surface waves propagating between pairs of stations by computing crosscorrelation for visualization or monitoring 29,30 . Identifying dominant anthropogenic noise helps explore geophysics using passive seismic noise.…”
Section: Discussionmentioning
confidence: 99%