Gongola Basin Geoid Determination using Isostatic Models and Seismic Reflection Data and Geophysical Interpretation
© E.E. Epuh, J.B. Olaleye, O.G. Omogunloye, 2016
The application of Stokes' formula to create geoid undulation requires no masses outside the geoid. Usually, a constant density
of 2.67 g/cm3 is used in the determination of the geoid which introduces error in the reduced gravity anomalies
and consequently the geoid. In this paper, isostatic models of Airy-Heiskanen and Pratt-Hayford were utilized in the determination of the geoid
by considering the planar and spherical approximation models the indirect effect of the topographic lateral density variation on the geoid was
computed as additive correction for the improvement of the accuracy of the computed geoid. Additional density information deduced from
seismic and well log information were considered for the variable density computation. The geopotential geoid undulations were computed from
the EGM 2008 model. The residual geoid was obtained by subtracting the local isostatic geoid from the geopential geoid. Geoid and gravity
admittance studies were also carried out to complement the results from the residual geoid.
Key word: geoid undulation, Airy-Heiskanen model, Pratt-Hayford model, isostatic residual gravity anomaly, residual geoid undulation.
The planar and spherical approximation results showed similar characteristics; but a change in magnitude in both models. Our results
suggest that the effects of topographic lateral density variations in geoid determination are significant and should be considered in rift basins.
The geophysical analysis of the geoid results show that the north-east has positive residual geoid which indicates the presence of high density
intrusive igneous rocks, while the south-east has negative residual geoid which indicates the dominant presence of low density sedimentary rocks.
The results also show that the radial distribution of the anomalous mass obtained using the geoid/residual geoid anomaly uniquely matched
that obtained using the seismic reflection data which inferred the presence of hydrocarbon accumulation in the southeast zone of the project area.
The gravity and geoid admittance studies corroborated the residual geoid and seismic reflection results.