The process of prestack migration of a 2D seismic data set using equivalent offset and CSP gathers creates an intermediate collection of traces- the CSP gather- that can easily be sorted and stacked to create an unmigrated section. Creation of the unmigrated section is insensitive to velocity except at steep dips. Thus the unmigrated equivalent offset section may be the ideal brute stack. In the process of full prestack time migration using the equivalent offset method, the unmigrated stack is useful for the identification of seismic events and structure for velocity analysis. An unmigrated stack of a portion of the Marmousi model created with a single velocity function compares well with the best unmigrated section created by one of the or...
The fundamental of the thesis is to improve the synthetic seismic data using a migration technique....
True-amplitude migration and demigration are two familiar processes in the world of seismic imaging....
We routinely image seismic data beyond the usual Nyquist sampling limits when we stack into limited-...
A method of prestack time migration is presented that is simpler, faster, and provides better veloci...
All the conventional methods for residual statics analysis require normal moveout (NMO) correction a...
The quality of the final image from the usual approach to 3-D prestack time migration is often compr...
A new technique for imaging 3-D prestack seismic reflection data has been developed. This method app...
In 3D seismics offset is a vector characterized by the source-receiver distance and azimuth. Due to ...
Most of the migration techniques require an input velocity model. Velocity analysis is one of the mo...
Abstract in UndeterminedWe introduce a new method for prestack depth migration of seismic common-sho...
The 1970\u27s saw the introduction and development of post-stack migration algorithms to the extent ...
Information about seismic velocities is an important and integral part of the seismic imaging proces...
Prestack Depth Migrated (PSDM) sections are the final results of a whole seismic acquisition and pro...
Prestack migration methods based on data binning pro-duce kinematic artifacts, i.e. coherent events ...
Introduction Prestack depth migration algorithms are usually divided into two classes: wavefield ex...
The fundamental of the thesis is to improve the synthetic seismic data using a migration technique....
True-amplitude migration and demigration are two familiar processes in the world of seismic imaging....
We routinely image seismic data beyond the usual Nyquist sampling limits when we stack into limited-...
A method of prestack time migration is presented that is simpler, faster, and provides better veloci...
All the conventional methods for residual statics analysis require normal moveout (NMO) correction a...
The quality of the final image from the usual approach to 3-D prestack time migration is often compr...
A new technique for imaging 3-D prestack seismic reflection data has been developed. This method app...
In 3D seismics offset is a vector characterized by the source-receiver distance and azimuth. Due to ...
Most of the migration techniques require an input velocity model. Velocity analysis is one of the mo...
Abstract in UndeterminedWe introduce a new method for prestack depth migration of seismic common-sho...
The 1970\u27s saw the introduction and development of post-stack migration algorithms to the extent ...
Information about seismic velocities is an important and integral part of the seismic imaging proces...
Prestack Depth Migrated (PSDM) sections are the final results of a whole seismic acquisition and pro...
Prestack migration methods based on data binning pro-duce kinematic artifacts, i.e. coherent events ...
Introduction Prestack depth migration algorithms are usually divided into two classes: wavefield ex...
The fundamental of the thesis is to improve the synthetic seismic data using a migration technique....
True-amplitude migration and demigration are two familiar processes in the world of seismic imaging....
We routinely image seismic data beyond the usual Nyquist sampling limits when we stack into limited-...