In porous, fluid-filled rock formations, compressional seismic wave velocities show a strong dependence on frequency. The potential linkage between P-wave velocity dispersion and permeability would make the use of broadband sonic waveform data suitable for determining reservoir parameters. Automatic velocity analysis of multi-channel sonic data can be tailored to detect and measure frequency dependent velocities.This seismic data processing strategy enables the creation of velocity dispersion logs for fluid-filled porous media
Laboratory measurements of the attenuation and velocity dispersion of compressional and shear waves ...
These data are the P- and S-wave velocities obtained by Ba et al. through ultrasonic experimental me...
The influence of fluid mobility on seismic velocity dispersion is directly observed in laboratory me...
Permeability is a key parameter for the evaluation of subsurface formations in groundwater and hydro...
My dissertation focuses on establishing a link between the rock heterogeneities and the fluid flow-r...
Fluid saturated rocks exhibit a dependence of acoustic velocities on frequency, which is called ve...
Fluid saturated rocks exhibit a dependence of acoustic velocities on frequency, which is called velo...
Typical rock samples with different lithologic characteristics were collected from exploring wells d...
Fluid saturated rocks exhibit a dependence of acoustic velocities on frequency, which is called velo...
Full waveform sonic logging, with the transmitter set at different centre frequencies, often provide...
Laboratory measurements of the attenuation and velocity dispersion of compressional and shear waves ...
Laboratory measurements of the attenuation and velocity dispersion of compressional and shear waves ...
These data are the P- and S-wave velocities obtained by Ba et al. through ultrasonic experimental me...
Laboratory measurements of the attenuation and velocity dispersion of compressional and shear waves ...
Velocities of seismic compressional and shear waves in porous rocks under different saturation condi...
Laboratory measurements of the attenuation and velocity dispersion of compressional and shear waves ...
These data are the P- and S-wave velocities obtained by Ba et al. through ultrasonic experimental me...
The influence of fluid mobility on seismic velocity dispersion is directly observed in laboratory me...
Permeability is a key parameter for the evaluation of subsurface formations in groundwater and hydro...
My dissertation focuses on establishing a link between the rock heterogeneities and the fluid flow-r...
Fluid saturated rocks exhibit a dependence of acoustic velocities on frequency, which is called ve...
Fluid saturated rocks exhibit a dependence of acoustic velocities on frequency, which is called velo...
Typical rock samples with different lithologic characteristics were collected from exploring wells d...
Fluid saturated rocks exhibit a dependence of acoustic velocities on frequency, which is called velo...
Full waveform sonic logging, with the transmitter set at different centre frequencies, often provide...
Laboratory measurements of the attenuation and velocity dispersion of compressional and shear waves ...
Laboratory measurements of the attenuation and velocity dispersion of compressional and shear waves ...
These data are the P- and S-wave velocities obtained by Ba et al. through ultrasonic experimental me...
Laboratory measurements of the attenuation and velocity dispersion of compressional and shear waves ...
Velocities of seismic compressional and shear waves in porous rocks under different saturation condi...
Laboratory measurements of the attenuation and velocity dispersion of compressional and shear waves ...
These data are the P- and S-wave velocities obtained by Ba et al. through ultrasonic experimental me...
The influence of fluid mobility on seismic velocity dispersion is directly observed in laboratory me...