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The Saturation Modelling workflow provides a fast, QI-based approach to evaluating whether seismic amplitude variations can reliably distinguish fluid and lithology effects in a given geological setting. By integrating fluid and mineral mixing models, Gassmann-based rock physics, and synthetic gather generation, the workflow enables interpreters to test seismic responses and assess detectability before committing to detailed quantitative interpretation.
This early-stage screening is critical in exploration, helping to understand what the seismic can tell us and reduce the risk of false amplitude-based prospectivity.
