International audienceRayleigh wave ellipticity as a function of frequency is closely linked to underground structure, i.e., shear wave velocity profile and sediment thickness. The possibility to calculate these underground properties by inverting ellipticity curves has recently been shown. We propose a new technique enabling the Rayleigh wave ellipticity to be recovered over a wide frequency range by using ambient noise recordings. Based on the random decrement technique commonly used to characterize dynamic parameters of buildings, this method eliminates all wave types except Rayleigh waves. We apply the method to noise synthetics simulated for different underground structures and show its applicability to real seismic noise data
The Mw 6.0 earthquake that hit central Italy on 24 August 2016 caused an abnormally high level of de...
International audienceWe demonstrate that the coherent information about the Earth structure can be ...
Slope stability analysis in seismically active areas must take into consideration the influence of s...
International audienceRayleigh wave ellipticity as a function of frequency is closely linked to unde...
The local soil structure (i.e. shear and pressure wave velocities) can be obtained by inversion of d...
We develop a new method for measuring ellipticity of Rayleigh waves from ambient noise records by de...
International audienceDispersion curves of surface waves, i.e., the wave velocity as a function of f...
The knowledge of the local soil structure is important for the assessment of seismic hazards. A wide...
We develop a new method for measuring ellipticity of Rayleigh waves from ambient noise records by de...
Several methods have been proposed in the past years to extract the Rayleigh wave ellipticity from h...
The sediments underlying the city of Lucerne (Switzerland) consisting of fluvio-lacustrine deposits ...
Spectral amplitude ratios between horizontal and vertical components (H/V ratios) from seismic recor...
Passive recordings of seismic noise are increasingly used in earthquake engineering to measure in si...
In the last few decades, we have witnessed a growing awareness of the role of site dynamic response ...
National audienceAmbient vibration techniques such as the H/V method may have the potential to signi...
The Mw 6.0 earthquake that hit central Italy on 24 August 2016 caused an abnormally high level of de...
International audienceWe demonstrate that the coherent information about the Earth structure can be ...
Slope stability analysis in seismically active areas must take into consideration the influence of s...
International audienceRayleigh wave ellipticity as a function of frequency is closely linked to unde...
The local soil structure (i.e. shear and pressure wave velocities) can be obtained by inversion of d...
We develop a new method for measuring ellipticity of Rayleigh waves from ambient noise records by de...
International audienceDispersion curves of surface waves, i.e., the wave velocity as a function of f...
The knowledge of the local soil structure is important for the assessment of seismic hazards. A wide...
We develop a new method for measuring ellipticity of Rayleigh waves from ambient noise records by de...
Several methods have been proposed in the past years to extract the Rayleigh wave ellipticity from h...
The sediments underlying the city of Lucerne (Switzerland) consisting of fluvio-lacustrine deposits ...
Spectral amplitude ratios between horizontal and vertical components (H/V ratios) from seismic recor...
Passive recordings of seismic noise are increasingly used in earthquake engineering to measure in si...
In the last few decades, we have witnessed a growing awareness of the role of site dynamic response ...
National audienceAmbient vibration techniques such as the H/V method may have the potential to signi...
The Mw 6.0 earthquake that hit central Italy on 24 August 2016 caused an abnormally high level of de...
International audienceWe demonstrate that the coherent information about the Earth structure can be ...
Slope stability analysis in seismically active areas must take into consideration the influence of s...