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- W2007183774 abstract "Reconnaissance gravity surveys carried out in the Benue Trough from 1975 to 1977 have revealed a broad positive regional anomaly over the whole trough attributable to Moho uplift. Superimposed on this regional gravity high in the Lower Benue Trough is an axial positive anomaly. This positive anomaly, with a maximum width of 100 km and an amplitude of 20 mGal, seems to disappear around latitude 9°N, and is associated with a basic body of density 2.90 gcm−3 that decreases in width and thickness from the south to the north. An axial negative anomaly observed in the Upper Benue is attributed to sedimentary fill, 6000 m thick. In the Middle and Lower Benue, flanking negative anomalies are attributable to the accumulation in the marginal basins of post deformational sediments up to 5000 m thick." @default.
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- W2007183774 date "1981-10-01" @default.
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- W2007183774 title "A gravity interpretation of the Benue trough, Nigeria" @default.
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- W2007183774 doi "https://doi.org/10.1016/0040-1951(81)90235-3" @default.
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