With the purpose of characterizing the Earth subsurface, one of the objectives of the inversion of prestack seismic data is to determine contrasts between rock properties from the information contained in the variation of the amplitudes of the reflected compressional waves with the angle of incidence. This amplitude-versus-angle (AVA) variation can be described by various approximations to the so-called Zoeppritz equations, a set of non-linear equations that depend on the physical characteristics of the medium at each side of the interface where the compressional wave strikes. The coefficients of such approximations constitute AVA attributes that may provide important information about fluid content, a key issue for the characterization of ...
Trace inversion for reservoir parameters is affected by angle averaging of seismic data and wavelet ...
We present an algorithm to estimate blocky images of the subsurface acoustic impedance (AI) from pos...
Resolving thin layers and achieve focused layer boundaries is one of the major challenges in seismic...
With the purpose of characterizing the Earth subsurface, one of the objectives of the inversion of p...
A new inversion method to estimate high-resolution amplitude-versus-angle attributes (AVA) attribute...
Seismic data contain information regarding the phase and amplitude of reflected events. Variations i...
To estimate rock and pore-fluid properties of oil and gas reservoirs in the subsurface, techniques c...
The study and interpretation of hydraulically stimulated regions, such as certain unconventional hyd...
We present a new inversion method to estimate, from prestack seismic data, blocky P- and S-wave velo...
International audienceA seismic processing workflow based on iterative migration/inversion and targe...
Wavelet estimation, ray tracing, and traveltime inversion are fundamental problems in seismic explo...
The sparse spike inversion method estimates from deconvolved seismic data that reflectivity which ha...
To overcome the weaknesses of conventional prestack amplitude variation with angle inversion based o...
Sparse spikes deconvolution is one of the oldest inverse problems, which is a stylized version of re...
A seismic processing workflow based on iterative ray + Born migration/inversion and target-oriented ...
Trace inversion for reservoir parameters is affected by angle averaging of seismic data and wavelet ...
We present an algorithm to estimate blocky images of the subsurface acoustic impedance (AI) from pos...
Resolving thin layers and achieve focused layer boundaries is one of the major challenges in seismic...
With the purpose of characterizing the Earth subsurface, one of the objectives of the inversion of p...
A new inversion method to estimate high-resolution amplitude-versus-angle attributes (AVA) attribute...
Seismic data contain information regarding the phase and amplitude of reflected events. Variations i...
To estimate rock and pore-fluid properties of oil and gas reservoirs in the subsurface, techniques c...
The study and interpretation of hydraulically stimulated regions, such as certain unconventional hyd...
We present a new inversion method to estimate, from prestack seismic data, blocky P- and S-wave velo...
International audienceA seismic processing workflow based on iterative migration/inversion and targe...
Wavelet estimation, ray tracing, and traveltime inversion are fundamental problems in seismic explo...
The sparse spike inversion method estimates from deconvolved seismic data that reflectivity which ha...
To overcome the weaknesses of conventional prestack amplitude variation with angle inversion based o...
Sparse spikes deconvolution is one of the oldest inverse problems, which is a stylized version of re...
A seismic processing workflow based on iterative ray + Born migration/inversion and target-oriented ...
Trace inversion for reservoir parameters is affected by angle averaging of seismic data and wavelet ...
We present an algorithm to estimate blocky images of the subsurface acoustic impedance (AI) from pos...
Resolving thin layers and achieve focused layer boundaries is one of the major challenges in seismic...