Abstract

Deepwater environment of Mahanadi basin in the Mio-Pliocene window is dominated by mud prone channel system. Sandstone reservoir of channel-levee complexes in this window are transported from the shelfal environment in the north to the basinal part in the south. Stratigraphic features of channel-levee complexes in the study area of deep water of Mahanadi basin are mapped by seismic amplitude in the Mio-Pliocene window because of the acoustic impedance contrast between reservoir and non-reservoir facies. Different inversion attributes are modeled and cross-plotted using the rock physics model of well