A Deterministic Evaluation of eismic Fidelity using Velocity Modeling ...
A Deterministic Evaluation of eismic Fidelity using Velocity Modeling ...
A Deterministic Evaluation of eismic Fidelity using Velocity Modeling ...
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Chapter 6<br />
Interpretation<br />
6.1 Introduction<br />
Improvements I made to enhance the s<strong>eismic</strong> image positively impacted data in several<br />
ways. One <strong>of</strong> the more significant improvements was providing information that<br />
permitted a higher degree <strong>of</strong> interpretation accuracy. As a final measure to assess an<br />
increase in fidelity I interpreted the data to determine if more geologic information could<br />
be gleaned. I used coherence to demonstrate an improved migration over the PSTM, data<br />
that were also valuable as an interpretation tool. I compared common image gathers<br />
(CIGs), the fidelity <strong>of</strong> the s<strong>eismic</strong> sections, and well ties to the s<strong>eismic</strong> for QC. Using all<br />
<strong>of</strong> the various criteria for improvement I determined that the data generated <strong>using</strong> well<br />
velocities were better suited for interpretation than those from semblance velocities.<br />
Objectives for the interpretation were to further verify improved fidelity by providing a<br />
more detailed interpretation and to gain new insights into the geologic processes<br />
associated with Vinton Dome. I used two benchmarks to evaluate improvements in<br />
interpretation. One was imaging near the flanks <strong>of</strong> the dome assessed by higher accuracy<br />
in identifying the truncation <strong>of</strong> sediments on the flanks <strong>of</strong> the salt dome. Identification <strong>of</strong><br />
small faults was the second benchmark I used in evaluation and well ties were used as a<br />
guide in interpretation.<br />
A more general objective was to gain insights into the geology surrounding Vinton<br />
Dome. Three areas <strong>of</strong> interest were investigated, salt tectonics, stratigraphy, and<br />
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