Al-Hikmah University Journal

The Borno Basin is located in North-Eastern Nigeria, formed in the Early Cretaceous.

Deposition of sediments in the basin occurred during rifting. The sediments are mainly

lacustrine shales and sandstones. This work was undertaken by the integration of 3D seismic

interpretations and the well data analysis of eight wells fairly distributed in the study area to

determine the thickness of the formations within the sub-basin. Da-1 well used in this study

was subdivided into stratigraphic units based on the regional stratigraphic subdivision of the

Chad basin and was later correlated with other wells using the similarity of observed log

responses. Density and sonic logs were used to generate synthetic seismograms for seismic to

well ties. Five horizons were interpreted, representing the tops of the formations on the 3D

seismic data covering the block, average velocity function with a maximum residual of 0.48%

was used for the time to depth conversion in all the generated maps. There is a general

thickening of sediments from the west to the east and the estimated thicknesses of the various

Formations in the Baga/Lake sub-basin are; Chad (400-750 m), Kerri-Kerri (300-1200 m),

Fika (300-1000 m) and Gongila (100-1300 m). The thickness of the Bima Formation could

not be established because the deepest well terminates within the Formation. This is a

modification to the previous and widely referenced studies of over fifty decades that based the

estimation of formation th