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The results of a seismic inversion method designed to screen for AVA anomalies in siliciclastic frontier basins is tested in a mature deep-water setting, the Mississippi Canyon, Gulf of Mexico. The method, which is founded on a universal rock property model for siliciclastic sediments, uses widely available partial stacks to invert seismic data for intercept and gradient impedances and generate a relative elastic inversion volume (rEEI), optimised for lithology and fluid detection. The results demonstrate the method is highly effective, but not infallible, at identifying hydrocarbons without any well data control in the simply buried Neogene and Paleogene (Tertiary) strata of the Mississippi Canyon. They further suggest that the use of the method in the early stages of prospecting in simply buried, siliciclastic basins globally, has the potential to identify opportunities that might otherwise be overlooked when interpreting only on the full stack.