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Gravity study of Lower Benue Trough, Nigeria

Published online by Cambridge University Press:  01 May 2009

C. I. Adighije
C. I. Adighije
Affiliation:
Gulf Oil Company (Nigeria) Limited, Private Mail Bag 2469, Lagos, Nigeria
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Summary

About 300 gravity stations were established at 2–4 km intervals along an E-W profile across the Lower Benue Trough from Gboko-Nsukka-Auchi with the main objectives of investigating the nature and configuration of the basement complex underlying the trough and estimating the thickness of the sedimentary cover rocks. The resulting Bouguer anomaly profile shows a series of alternating positives and negatives. For a preliminary interpretation, the positive anomalies are attributed to shallow basement and the negative anomalies to sediment-fill of maximum thickness, 4250 m.

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Type
Articles
Information
Geological Magazine , Volume 118 , Issue 1 , January 1981, pp. 59 - 67
Copyright
Copyright © Cambridge University Press 1981

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References

Ajakaiye, D. E. 1972. A table of theoretical gravity values between the equator and latitude 18°. Nig. Jl Min. Geol. 7 43–87.Google Scholar
Burke, K., Dessauvagie, T. & Whiteman, A. J. 1971. Opening of the Gulf of Guinea and the geological history of the Benue Depression and Niger Delta. Nature, Lond. 233 51–5.Google Scholar
Burke, K., Dessauvagie, T. & Whiteman, A. J. 1972. Geological history of the Benue Valley and adjacent areas. In African Geology, Vol. 1 (ed. Dessauvagie, T. F. and Whiteman, A. J.), pp. 187–205. Nigeria: Ibadan University Press.Google Scholar
Cratchley, C. & Jones, G. P. 1965. An interpretation of the geology and gravity anomalies of the Benue Valley, Nigeria. Overseas geol. Surv. Geophys. Paper 1.Google Scholar
Farrington, J. L. 1952. Preliminary description of the Nigerian lead-zinc field. Econ. Geol. 47 583–608.CrossRefGoogle Scholar
Grant, N. K. 1971. Sough Atlantic, Benue Trough and Gulf of Guinea triple junction. Bull. geol. Soc. Am. 82 2295–8.Google Scholar
Hammer, S. 1974. Approximation in gravity interpretation calculation. Geophysics 39 205–22.CrossRefGoogle Scholar
Kane, M. F. 1962. Comprehensive system of terrain corrections using a digital computer. Geophysics 27 455–62.Google Scholar
Kogbe, C. A. 1976. The Cretaceous and Paleogene sediments of Southern Nigeria. In Geology of Nigeria, Vol. 1 (ed. Kogbe, C. A.), pp. 273–82. Lagos: Elizabethan Co.Google Scholar
Lukavchenko, P. I. 1951. Calculation of topographic corrections from tables and nomograms. In Gravity Prospecting (ed. Sazhina, N. & Grunshinsky, N.), pp. 64–96. Moscow: MIR.Google Scholar
Nettleton, L. L. 1942. Geophysical prospecting for oil, pp. 16–148. London: McGraw-Hill.Google Scholar
Nwachukwu, S. O. 1972. The tectonic evolution of the southern portion of the Benue Trough, Nigeria. Geol. Mag. 109 411–19.Google Scholar
Nwachukwu, S. O. 1975. Temperature of formation of vein minerals in the southern portion of the Benue Trough, Nigeria. Nig. Jl Min. Geol. 11 45–55.Google Scholar
Olade, M. A. 1975. Evolution of Nigeria's Benue Trough (aulacogen): a tectonic model. Geol. Mag. 112 575–83.Google Scholar
Uzuakpunwa, A. B. 1974. The Abakaliki pyroclastics, Eastern Nigeria: new age and tectonic implications. Geol. Mag. 111 65–70.CrossRefGoogle Scholar
Wright, J. B. 1968. South Atlantic continental drift and the Benue Trough. Tectonophys. 6 301–310.Google Scholar