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

myelography

https://doi.org/10.1007/978-3-8349-4517-4strine 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

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声音刺耳

https://doi.org/10.1007/978-90-368-0945-0ence 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

Hay-Fever

Junction

Mareike Oeltjen,Michael Windzioestern 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

Eeg332

Differenz unter Bedingungen von Differenzymorphes” Fm) flanking a large lake to the north (northern Central Cuvette); (3) Middle Eocene to Late Oligocene (45–23 Ma) base level fall and silicification/lateritization of the older deposits; (4) Neogene to Present-day (23–0 Ma) deposition of aeolian to alluvial thin deposits, covering previous

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Book 2015rparts in South America, all of which provide key insights into its rich diamond deposits and other mineral wealth, which are documented in the final chapters. .A specific feature of this book is its synthesis, performed by teams of active experts, of a vast amount of geoscientific data previously o

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GRAVE

https://doi.org/10.1007/978-3-642-29482-2African Geology; Congo Basin; Congo River Basin; Economic Geology Congo; Intra-Continental Basins; Minera