Titlebook: Geology and Resource Potential of the Congo Basin; Maarten J. de Wit,Fran?ois Guillocheau,Michiel C. Book 2015 Springer-Verlag Berlin Hei

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New Regional Correlations Between the Congo, Paraná and Cape-Karoo Basins of Southwest Gondwanaestern margin of Gondwana linked the Paraná Basin with the Cape-Karoo Basin of South Africa. Equivalent sequences are absent in the Congo Basin. In contrast, succeeding Carboniferous-Permian and Triassic successions are similar in all the Congo, Paraná and Cape-Karoo Basins, including thick transgre

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expository

https://doi.org/10.1007/978-3-663-16057-1ing suggests that lithospheric structure beneath the basin is not uniform, as is commonly assumed in geodynamic models explaining how the basin formed. A second geodynamic implication concerns the Neoproterozoic rifting event that may have initiated basin subsidence. The proposed locations of the ri

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https://doi.org/10.1007/978-3-663-16058-8rlites and a number of complex Archean Cratons that outcrop along the flanks of the CB. The CB of central Africa is underlain and completely surrounded by peneplained Precambrian basement that spans a history more than 3.6 Ga, including rocks along its northeastern edge possibly as old as 4.0 Ga, se

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Core Books in Advanced Mathematicsn the matrix. Detailed observation of the solution cavities suggests three distinct stages of formation: (1) incipient fungal colonization, physical penetration of primary carbonate grains boundaries by penetrating fungal stolons, (2) EPS production, organic acid dissolution and neomineral formation

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The Development of the Cells of the Blood,, possibly related to late Paleozoic intracontinental deformation associated with the Mauritanian-Variscan and Cape-de la Ventana orogens flanking the northwestern and southern margins of Gondwana, respectively. This change in basin paleogeography is consistent with detrital zircons dated from these

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