Add to ORKGThe current work focuses on a new method for generating theoretical dispersion curves for Rayleigh wave propagation that is consistent with the common frequency-wavenumber (f-k) technique typically used to determine the experimental dispersion relation. The method considers all possible Rayleigh modes, and will be the basis for an inversion procedure that will lead to the determination of the shear wave velocity profile for any layered system
The knowledge of the local soil structure is important for the assessment of seismic hazards. A wide...
Rayleigh-wave dispersion is observed every time acoustic impedance stratification occurs, and its an...
A seismic survey was carried out on a tidal flat in the SW-Netherlands in order to determine shear-w...
Abstract. Rayleigh wave or ground roll is a noise in seismic body waves. However, how to use this no...
Inversion of the fundamental mode of the Rayleigh wave dispersion curve does not provide a unique so...
International audienceInversion of the fundamental mode of the Rayleigh wave dispersion curve does n...
A method has been presented to establish the theoretical dispersion curve for performing the inverse...
The shear (S)-wave velocity of near-surface materials (such as soil, rocks, and pavement) and its ef...
The Rayleigh-wave phase velocity of a layered earth model is a function of frequency and four groups...
In case of irregular dispersive media, a proper analysis of higher modes existing in a dispersion pl...
Rayleigh wave dispersion data usually appear in the form of multimodal spectra for a layered model s...
The Spectral-Analysis-of-Surface-Waves (SASW) method is a seismic method for measuring in situ elast...
Rayleigh-wave propagation in a layered, elastic earth model is frequency-dependent (dispersive) and ...
The phase velocity of Rayleigh-waves of a layered earth model is a function of frequency and four gr...
An attempt to discuss and/or verify the suitability of subsoil velocity models estimated from Monte-...
The knowledge of the local soil structure is important for the assessment of seismic hazards. A wide...
Rayleigh-wave dispersion is observed every time acoustic impedance stratification occurs, and its an...
A seismic survey was carried out on a tidal flat in the SW-Netherlands in order to determine shear-w...
Abstract. Rayleigh wave or ground roll is a noise in seismic body waves. However, how to use this no...
Inversion of the fundamental mode of the Rayleigh wave dispersion curve does not provide a unique so...
International audienceInversion of the fundamental mode of the Rayleigh wave dispersion curve does n...
A method has been presented to establish the theoretical dispersion curve for performing the inverse...
The shear (S)-wave velocity of near-surface materials (such as soil, rocks, and pavement) and its ef...
The Rayleigh-wave phase velocity of a layered earth model is a function of frequency and four groups...
In case of irregular dispersive media, a proper analysis of higher modes existing in a dispersion pl...
Rayleigh wave dispersion data usually appear in the form of multimodal spectra for a layered model s...
The Spectral-Analysis-of-Surface-Waves (SASW) method is a seismic method for measuring in situ elast...
Rayleigh-wave propagation in a layered, elastic earth model is frequency-dependent (dispersive) and ...
The phase velocity of Rayleigh-waves of a layered earth model is a function of frequency and four gr...
An attempt to discuss and/or verify the suitability of subsoil velocity models estimated from Monte-...
The knowledge of the local soil structure is important for the assessment of seismic hazards. A wide...
Rayleigh-wave dispersion is observed every time acoustic impedance stratification occurs, and its an...
A seismic survey was carried out on a tidal flat in the SW-Netherlands in order to determine shear-w...