Dip MoveOut (DMO) and Azimuth MoveOut (AMO) are considered in a general framework which allows for lateral variations in the velocity model, including variations which generate caustics in the wavefield. DMO and AMO are constructed through the composition of operators in a general velocity model, using the scattering angle and azimuth parameterisation [4]. In this parameterisation, impulse responses analogous to DMO and AMO are computed in a the gas lens model presented in [5]. The results clearly show how errors can be introduced by assuming, for example, a constant velocity gradient model when the true model is laterally heterogeneous
A robust method for estimating the interval parameters (i. e. the normal move-out velocity Vnmo and ...
textWe are concerned with forward wave motion simulations in two-dimensional elastic, heterogeneous,...
Wavefield extrapolation for a laterally varying velocity model can be achieved by applying a nonstat...
Dip moveout (DMO) and azimuth moveout (AMO) are considered in a general framework that allows for la...
Reflection seismic data continuation is the computation of data at source and receiver locations tha...
The standard NMO equation for a seismic reflection from a flat interface within a homogeneous, isotr...
In this paper, we present a new method of normal move-out (NMO) correction that works on a trace by ...
Robust estimation of anisotropy parameters is one of the most important problems in seismic imaging ...
We propose a novel directional decomposition operator for wavefield snapshots in heterogeneous-veloc...
Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Conselho Nacional de Desenvolvime...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
Oil, gas, and geothermal reservoirs, and overlying strata are often composed of anisotropic rocks. P...
Conventional amplitude-versus-offset (AVO) analysis such as linear fitting of isotime samples after ...
While in the past, in the context of stacking, traveltime moveout was only formulated in individual ...
Abstract. Transverse isotropy with a vertical symmetry axis (VTI media) is the most common anisotrop...
A robust method for estimating the interval parameters (i. e. the normal move-out velocity Vnmo and ...
textWe are concerned with forward wave motion simulations in two-dimensional elastic, heterogeneous,...
Wavefield extrapolation for a laterally varying velocity model can be achieved by applying a nonstat...
Dip moveout (DMO) and azimuth moveout (AMO) are considered in a general framework that allows for la...
Reflection seismic data continuation is the computation of data at source and receiver locations tha...
The standard NMO equation for a seismic reflection from a flat interface within a homogeneous, isotr...
In this paper, we present a new method of normal move-out (NMO) correction that works on a trace by ...
Robust estimation of anisotropy parameters is one of the most important problems in seismic imaging ...
We propose a novel directional decomposition operator for wavefield snapshots in heterogeneous-veloc...
Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Conselho Nacional de Desenvolvime...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
Oil, gas, and geothermal reservoirs, and overlying strata are often composed of anisotropic rocks. P...
Conventional amplitude-versus-offset (AVO) analysis such as linear fitting of isotime samples after ...
While in the past, in the context of stacking, traveltime moveout was only formulated in individual ...
Abstract. Transverse isotropy with a vertical symmetry axis (VTI media) is the most common anisotrop...
A robust method for estimating the interval parameters (i. e. the normal move-out velocity Vnmo and ...
textWe are concerned with forward wave motion simulations in two-dimensional elastic, heterogeneous,...
Wavefield extrapolation for a laterally varying velocity model can be achieved by applying a nonstat...