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Titlebook: Geology and Mineral Resources of West Africa; J. B. Wright,J. B. Wright Book 1985 J. B. Wright, D. A. Hastings, W. B. Jones & H. R. Willia

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樓主: 板條箱
41#
發(fā)表于 2025-3-28 16:16:25 | 只看該作者
42#
發(fā)表于 2025-3-28 21:49:55 | 只看該作者
The Precambrian of West Africa — synthesis and reviewowever, has had more to do with levels of erosion, relative abundance of different rock types, climatic changes, erosion levels and intensity of weathering than with the fundamentals of global tectonics. Rock associations remain the most important control on the occurrence of mineral deposits.
43#
發(fā)表于 2025-3-28 23:49:13 | 只看該作者
Economic potential of the younger sedimentary basins are generally not so large or abundant as in basement terranes, but include ores of lead, zinc, iron and manganese, and there may also be some bauxite. Smaller deposits of these various resources are already exploited on a small scale.
44#
發(fā)表于 2025-3-29 06:13:00 | 只看該作者
Allgemeine Schmerzen im Abdomen,coastal basins, the Senegal Basin is by far the largest, but the basins along the southern coast of West Africa are larger than their surface extents suggest, as substantial parts of their successions are offshore.
45#
發(fā)表于 2025-3-29 10:15:23 | 只看該作者
The Benue Trough and coastal basinscoastal basins, the Senegal Basin is by far the largest, but the basins along the southern coast of West Africa are larger than their surface extents suggest, as substantial parts of their successions are offshore.
46#
發(fā)表于 2025-3-29 14:13:16 | 只看該作者
47#
發(fā)表于 2025-3-29 15:57:01 | 只看該作者
48#
發(fā)表于 2025-3-29 21:41:24 | 只看該作者
,Solit?re Rundschatten der Lungen,ntial thickness of Quaternary sediments in the Chad Basin..Cretaceous marine sedimentation was of shallow-water type, depositing limestones, sandstones and shales, with lithologies and fossils that indicate generally warm climatic conditions throughout. Maximum sediment thicknesses in the lullmedden and Chad Basins are of the order of 2000–3000 m.
49#
發(fā)表于 2025-3-30 00:08:40 | 只看該作者
50#
發(fā)表于 2025-3-30 04:46:14 | 只看該作者
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