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- W2005432960 abstract "Recently, a model of the Standard African lithosphere was constructed using regional Bouguer anomalies (Brown and Girdler, 1980). Values of lithospheric and crustal thickness in this model are 100 km and 36.2 km, respectively. The corresponding value of Bouguer anomaly is —48 mgal. Bouguer anomalies of Uganda were averaged over 1° grids. They were found to range between −106 mgals and −160 mgals. Such values are probably associated with plateau and rift areas. The deviation of the lithospheric thickness in Uganda from that of the standard value was calculated using the difference between the averaged Bouguer anomaly at a given point and the standard one. The density contrast used is equal to −0.05gr/cm3. In this way it was possible to find the relation between the averaged Bouguer anomalies and lithosphere thickness in Uganda in the form: Hl=123+0.479 ΔgB(1°) Bouguer anomalies were also averaged over 15′ grids. The deviation of the crustal thickness at a given point from that of the standard value was calculated using the difference between values of Bouguer anomalies averaged over 1° and 15′ grids. A density contrast equal to +0.45 gr/cm3 was used. The relation between averaged Bouguer anomalies and crustal thickness in Uganda was deducted to be of the form: Hc=29.03−0.052 ΔgB(15′) From the given relations it was found that the thickness of the lithosphere in Uganda varies from 72 km in the central parts to 46 km in the eastern and western parts. On the other hand, the thickness of the crust was found to vary between 34 km in the central parts and 39 km in the eastern and western parts. Maps representing lithospheric and crustal thickness in Uganda are presented." @default.
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- W2005432960 title "Bouguer anomalies and lithosphere-crustal thickness in Uganda" @default.
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- W2005432960 doi "https://doi.org/10.1016/0264-3707(85)90027-4" @default.
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