Gas migration into the Mungaroo Formation is believed to have occurred through a combination of selective fault
and sand channel conduits, however, not all apparently sealed sandstone channels were charged, possibly
because of complete isolation from the migration fairway.Gas saturation in these sands is usually associated with
high seismic amplitudes, however, ambiguity exists due to high seismic amplitudes associated with high porosity brine
sands and also carbonaceous shales. This study outlines the comprehensive quantitative interpretation (QI) workflow
that was successful at identifying the gas bearing sands .