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The youngest Pleistocene leveed-channel fans of the Niger delta, offshore Nigeria, are defined by sea-bottom images and shallow reflection patterns in 2-D and 3-D seismic surveys. They make excellent analogues for interpreting older fans in the delta depocenter.

Niger delta structural trends control Pleistocene shelf, slope and basin depositional environments. The shelf margin is cut by canyons and gullies that are lowstand sediment paths to the basin. Upper slope areas, underlain by diapir and inner toe thrust structural trends, are zones of channel erosion and bypass. Lower slope areas, between the inner and outer thrust trends, contain leveed channels in local sags. They exhibit channel erosion and bypass in areas of active thrusts and tear faults.

The basin plain outboard of the outer thrust trend has major deposition of large leveed channel complexes. The central reentrant in the outer thrust trend is a major depocenter of leveed channels fed through a larger canyon. The area to the far northwest contains well-developed fans in the low area between the delta and the continental margin to the north.

A 3-D grid at the mouth of the large central canyon shows details of leveed channels deposited from the canyon. The first large sinuous channel was crevassed and abandoned by a smaller, straighter distributary near the canyon mouth. Slumping and mass transport are important elements, and are intimately involved in and adjacent to the channel systems.

The locations of fan complexes that comprise the deepwater depocenters appear directly related to the updip delta morphology and progradation of the fluvio-deltaic system.

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