The conventional seismic trace can be viewed as the real component of a complex trace which can be uniquely calculated under usual conditions. The complex trace permits the unique separation of envelope amplitude and phase information and the calculation of instantaneous frequency. These and other quantities can be displayed in a color-encoded manner which helps an interpreter see their interrelationship and spatial changes. The significance of color patterns and their geological interpretation is illustrated by examples of seismic data from three areas
textSeismic interpretation plays a crucial role in extracting geologic information from seismic imag...
Acquisition of 2D seismic profiles often serves as a prerequisite to the acquisition of the more rob...
Seismic data is difficult to analyze and classical mathematical tools reveal strong limitations in e...
Time-dependent amplitude and phase information of stacked seismic data are processed independently u...
A common theme in this thesis is the use of complex signal attributes to facilitate the processing, ...
The seismic trace is a complex aggregate of reflected and scattered signals from subsurface formatio...
Lateral changes in seismic phase can be used to detect small changes in seismic arrival time and wav...
Interpretation of seismic reflection data routinely involves powerful multiple-central-processing-un...
Traces files for all survey lines generated by processing the scanned images and a description of th...
The reflectivity series and resulting waveform for a generalized-simple layer (arbitrary reflection ...
<p>This figure represents the same signal, whose frequency increases to the right and intensity incr...
The interpreter who is used to conventional-resolution seismic data may be perplexed when confronted...
The location of seismic events can be improved if accurate picks can be assigned for later seismic p...
Improving the Accuracy of Digital Seismic Traces Generated from Images of Paper Sign Bit Seismic Sec...
A trained analyst can frequently provide a rapid assessment of a seismic record and provide identifi...
textSeismic interpretation plays a crucial role in extracting geologic information from seismic imag...
Acquisition of 2D seismic profiles often serves as a prerequisite to the acquisition of the more rob...
Seismic data is difficult to analyze and classical mathematical tools reveal strong limitations in e...
Time-dependent amplitude and phase information of stacked seismic data are processed independently u...
A common theme in this thesis is the use of complex signal attributes to facilitate the processing, ...
The seismic trace is a complex aggregate of reflected and scattered signals from subsurface formatio...
Lateral changes in seismic phase can be used to detect small changes in seismic arrival time and wav...
Interpretation of seismic reflection data routinely involves powerful multiple-central-processing-un...
Traces files for all survey lines generated by processing the scanned images and a description of th...
The reflectivity series and resulting waveform for a generalized-simple layer (arbitrary reflection ...
<p>This figure represents the same signal, whose frequency increases to the right and intensity incr...
The interpreter who is used to conventional-resolution seismic data may be perplexed when confronted...
The location of seismic events can be improved if accurate picks can be assigned for later seismic p...
Improving the Accuracy of Digital Seismic Traces Generated from Images of Paper Sign Bit Seismic Sec...
A trained analyst can frequently provide a rapid assessment of a seismic record and provide identifi...
textSeismic interpretation plays a crucial role in extracting geologic information from seismic imag...
Acquisition of 2D seismic profiles often serves as a prerequisite to the acquisition of the more rob...
Seismic data is difficult to analyze and classical mathematical tools reveal strong limitations in e...