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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書目名稱Geology and Resource Potential of the Congo Basin影響因子(影響力)




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熟練

Precambrian Basement of the Congo Basin and Its Flanking Terrainsrlites 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

譏諷

Sedimentology and Sequence Stratigraphy of the Late Precambrian Carbonates of the Mbuji-Mayi Supergrel of ca. 4 m, with fluctuations in the range around 1–4 m. This shallow-water depth and the abundance of cyanobacteria suggest that water column was oxygenated. By contrast the subtidal cyclic facies at the outer/middle ramp, preserve ‘thick’ subtidal sequences characterized by an average thickness

hypnogram

Probable Fungal Colonization and Carbonate Diagenesis of Neoproterozoic Stromatolites from South Gabn 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

花束

講個(gè)故事逗他

Paleogeography and Tectono-Stratigraphy of Carboniferous-Permian and Triassic ‘Karoo-Like’ Sequences, 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

講個(gè)故事逗他

Adjourn

Mesozoic Sedimentary Cover Sequences of the Congo Basin in the Kasai Region, Democratic Republic of strine deposits correlative to the Lukuga Group; (2) J1: Jurassic-age arid to semi-arid laminated shales and siltstones and aeolian sandstones, interpreted as ephemeral lake and sand dune sequences with interspersed loess deposits and rare fluvial channel sequences (considered part of the historic L

可能性

流出

Multiphase Phanerozoic Subsidence and Uplift History Recorded in the Congo Basin: A Complex Successoence during the Carboniferous-Triassic (10–20?m/Ma), and then slower subsidence during the Jurassic-Cretaceous (5–10?m/Ma), punctuated by several uplifts at 160–180?Ma (e.g. ‘Karoo’), 120–140?Ma (e.g. ‘Paraná-Etendeka’), and again in the Cenozoic, ca. 30–50?Ma (e.g. ‘Ethiopian’). This complex, multi