Limited by the poor seismic quality and few wells, it is full of challenge to delineate the distribution area and patterns of reservoir sands. The stratigraphy of this succession is composed of distributary channels, overbank, mouthbar and lacustrine shales.
The early Pliocene fan delta complex developed in the south of Lake Albert Basin which is located at the northern end of the western branch in the East African Rift System.
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