Bitumen, also known as oil sand, across Nigeria is hosted in the Eastern Dahomey Basin
spanning over several kilometers. Integration of five (5) traverses of 2D electrical resistivity
tomography (ERT), four (4) vertical electrical sounding (VES) and two (2) borehole
lithological logs have led to delineation of five geoelectric layers – namely topsoil, lateritic
soil, clay, shale/ marly limestone, bituminous sand and sandstone geoelectric units. The
bituminous sand is characterized with high resistivity value as contrast to previous values
obtained in other regions of the basin, ranging from 4177 Ωm to 70,000 kΩm with thickness
ranges from 15 m to 28m. 2D ERT shown that the bituminous sands occur within a relatively
shallow depth with a resistivity value ranging from 3225 Ωm to about 80,000 Ωm and a
thickness range of 5 to about 30m. The survey shown that bitumen occurrences are overlain
by relatively thin overburden (0-25m), and underlain by mudstone facies and limestone
facies. Similarly, relatively deeper bituminous sands have higher resistivity range and are
laterally continuous than the shallow occurrences. This suggests the sands comprising the
shallow and deeper occurrences are probably deposited under different geologic setting.