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

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Geology and Resource Potential of the Congo Basin978-3-642-29482-2Series ISSN 2364-6438 Series E-ISSN 2364-6446

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https://doi.org/10.1007/978-3-663-16057-1ral and southern Africa derived from an inversion of Rayleigh wave group velocity measurements. The model is similar to other tomographic models derived from Rayleigh wave phase velocities, revealing a region of fast upper mantle velocities in the 50–100 km depth interval beneath the northwestern, c

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https://doi.org/10.1007/978-3-658-39082-2sents a classic late Precambrian carbonate sequence whose architecture is poorly known. Here we present new data and synthesis of microfacies analysis, sequence stratigraphy, Fischer plots coupled with C and O isotopes, to evaluate the paleoecology and sea level variations of the carbonate series of

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Core Books in Advanced Mathematicsed solution cavities infilled with 0.1–3.0 μm-thick filamentous microbe-like structures, rhombohedral dolomite and quadratic-shaped dolomite crystals that may originally have been oxalates. The filaments appear entangled within an amorphous, organic matrix reminiscent of microbial extracellular poly

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The Development of the Cells of the Blood,sins of southern Gondwana. Here, we present a substantially revised stratigraphy for the Congo Basin, based on new field observations, seismic and borehole data, together with paleontology and new geochronology. In the center of the basin, the deepest boreholes intercept 3 to 4 km thick successions

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,Durchführung der Untersuchung,s a unique record of the tectonic and climatic evolution of central Africa during the main period of break-up of Gondwana and the emergence of the Indian and South Atlantic Oceans. New facies analysis and detailed correlations of these ‘Congo’ sequences are described from field observations in the s