effects on exploration seismic data both on land and offshore surveying. Ground roll (Rayleigh waves) and mud roll (Scholte waves) present in seismic records can be processed and inverted to supply a shear velocity model of the first hundreds meters. In this paper an automatic multimodal inversion for Rayleigh and Scholte waves using a new approach is presented. The proposed algorithm minimizes the L1 norm of the modulus of the Haskell-Thomson matrix determinant of the synthetic profile evaluated on real data. This algorithm is very fast, and it allows considering simultaneously all modes. Tests on both synthetic and real data, relative to Rayleigh and Scholte waves, have shown the importance of accounting for higher modes and the capabilit...
The inversion of Rayleigh-wave dispersion curves is a classic geophysical inverse problem. We have d...
Seismic data generated by a novel, seabed-coupled, shear-wave vibrator (prototype) and recorded by a...
Geophysical Inversion is an ill-posed problem that is inherently affected by the non-uniqueness of t...
Rayleigh wave or ground roll is a noise in seismic body waves. However, how to use this noise for so...
Near surface velocity models are needed for static corrections applied to seismic reflection data. S...
Shear wave velocity models can be built through surface wave analysis. For the presented field case,...
Recent studies have illustrated that the Multichannel Analysis of Surface Waves (MASW) method is an ...
Higher-mode contribution is important in surface-wave inversion because it allows more information t...
A study of surface-wave analysis can be divided into two main parts. In the first stage, dispersive ...
On land, surface waves are extensively and successfully used for the determination of Shear velocity...
Due to the character of seismic energy generation and propagation, shallow high-resolution seismic-r...
The joint inversion of Rayleigh wave dispersion and H/V curves from environmental noise measurements...
The shear (S)-wave velocity of near-surface materials (such as soil, rocks, and pavement) and its ef...
Acoustic propagation in littoral waters is greatly affected by seafloor sediment properties. Shear p...
The inversion of Rayleigh-wave dispersion curves is a classic geophysical inverse problem. We have d...
Seismic data generated by a novel, seabed-coupled, shear-wave vibrator (prototype) and recorded by a...
Geophysical Inversion is an ill-posed problem that is inherently affected by the non-uniqueness of t...
Rayleigh wave or ground roll is a noise in seismic body waves. However, how to use this noise for so...
Near surface velocity models are needed for static corrections applied to seismic reflection data. S...
Shear wave velocity models can be built through surface wave analysis. For the presented field case,...
Recent studies have illustrated that the Multichannel Analysis of Surface Waves (MASW) method is an ...
Higher-mode contribution is important in surface-wave inversion because it allows more information t...
A study of surface-wave analysis can be divided into two main parts. In the first stage, dispersive ...
On land, surface waves are extensively and successfully used for the determination of Shear velocity...
Due to the character of seismic energy generation and propagation, shallow high-resolution seismic-r...
The joint inversion of Rayleigh wave dispersion and H/V curves from environmental noise measurements...
The shear (S)-wave velocity of near-surface materials (such as soil, rocks, and pavement) and its ef...
Acoustic propagation in littoral waters is greatly affected by seafloor sediment properties. Shear p...
The inversion of Rayleigh-wave dispersion curves is a classic geophysical inverse problem. We have d...
Seismic data generated by a novel, seabed-coupled, shear-wave vibrator (prototype) and recorded by a...
Geophysical Inversion is an ill-posed problem that is inherently affected by the non-uniqueness of t...