Reservoir modelling sand-rich deep-water clastics: the necessity of down-scaling

Channels, lobes and levees are inadequate architectural elements to describ e sand body geometry in sand-rich deep-water systems. Sand sheets are the m ost common architectural element. Elutriation modifies primary sedimentary structures by mobilizing and reorganizing grains. This changes pore size di stribution and permeability characteristics. Bed amalgamation and offset st acking of sand sheets makes problematic the use of bed thickness in correla tion. A down-scaling approach for reservoir modelling is recommended, as a hierarchy of architectural elements that define up-scaling relationships ca nnot be established.