Herein, we expand and use the method used by Landa and Keydar (1998) to detect local heterogeneities. The method relies on computing local semblance along the diffraction offset-traveltime curves. We expand the method by taking into account the phase change occurring for edge diffractions. We demonstrate the usefulness of the method on hard-rock seismic data
Hard rock seismic exploration normally has to deal with rather complex geological environments. Thes...
Diffractions carry valuable information about local discontinuities and small scale objects in the s...
Discontinuities and small structures induce diffractions on seismic or ground-penetrating radar (GPR...
The primary objective of seismic exploration in a hard rock environment is the detection of heteroge...
Energy-angle distributions in the local image matrix, which is a function of local incident and rece...
Exploration for mineral deposits in a predominately hard rock environment is often quite difficult b...
textSeismic waves can either be reflected or diffracted by subsurface objects depending on the objec...
textSeismic waves can either be reflected or diffracted by subsurface objects depending on the objec...
One of the main objectives of seismic interpretation is the identification and positioning of struct...
In this work a robust imaging algorithm based on detecting edge diffraction has been developed. The ...
Many subsurface features, such as faults, fractures, cracks, or fluid content terminations are defin...
Many subsurface features, such as faults, fractures, cracks, or fluid content terminations are defin...
Diffracted waves are seismic waves that backscatter from localized discontinuities in the earth. The...
Diffracted waves are seismic waves that backscatter from localized discontinuities in the earth. The...
Hard rock seismic exploration normally has to deal with rather complex geological environments. Thes...
Hard rock seismic exploration normally has to deal with rather complex geological environments. Thes...
Diffractions carry valuable information about local discontinuities and small scale objects in the s...
Discontinuities and small structures induce diffractions on seismic or ground-penetrating radar (GPR...
The primary objective of seismic exploration in a hard rock environment is the detection of heteroge...
Energy-angle distributions in the local image matrix, which is a function of local incident and rece...
Exploration for mineral deposits in a predominately hard rock environment is often quite difficult b...
textSeismic waves can either be reflected or diffracted by subsurface objects depending on the objec...
textSeismic waves can either be reflected or diffracted by subsurface objects depending on the objec...
One of the main objectives of seismic interpretation is the identification and positioning of struct...
In this work a robust imaging algorithm based on detecting edge diffraction has been developed. The ...
Many subsurface features, such as faults, fractures, cracks, or fluid content terminations are defin...
Many subsurface features, such as faults, fractures, cracks, or fluid content terminations are defin...
Diffracted waves are seismic waves that backscatter from localized discontinuities in the earth. The...
Diffracted waves are seismic waves that backscatter from localized discontinuities in the earth. The...
Hard rock seismic exploration normally has to deal with rather complex geological environments. Thes...
Hard rock seismic exploration normally has to deal with rather complex geological environments. Thes...
Diffractions carry valuable information about local discontinuities and small scale objects in the s...
Discontinuities and small structures induce diffractions on seismic or ground-penetrating radar (GPR...