Abstract
Impedance models should be more than just the inversion of seismic data; they should result from the integration of data from diverse sources. This integration adds value to the impedance model by increasing the information content and interpretability of the various data. Often, the integration of geological, geophysical, and other data measured in the different domains of time and depth is not straightforward. One solution is to integrate the data within a common sequence stratigraphic framework.
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