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Multiphase Phanerozoic Subsidence and Uplift History Recorded in the Congo Basin: A Complex Successor Basin

Abstract : The Congo Basin of central Africa is a large iconic Phanerozoic sedimentary basin whose origin and tectonic evolution are poorly understood, mostly because of a lack of modern stratigraphic data, reflecting a long hiatus in field investigations during the past five decades. It is usually assumed that the Congo Basin experienced a long and continuous history of slow subsidence since the late Precambrian (e.g. 2–4 m/Ma), linked to steady-state mantle processes. Here, we used revised sedimentological and stratigraphic data of the four historic deep boreholes drilled in the center of the basin to calculate a new first-order model for its subsidence and uplift history. Because the sedimentary sequences of this basin are largely terrestrial, we apply a new backstripping method especially designed for continental domain. The results reveal two main episodes of subsidence: initially rapid subsidence 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, multiphase subsidence and uplift history of the Congo Basin can be linked to evolving far-field geodynamic processes that first led the formation of Pangea (large-scale compression) during the late Paleozoic, and then to its break-up associated with successive outpourings of Large Igneous Provinces (or hotspot plumes) and the opening of the Indian and South Atlantic Oceans around Africa.
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https://hal-insu.archives-ouvertes.fr/insu-01116954
Contributor : Isabelle Dubigeon <>
Submitted on : Monday, February 16, 2015 - 10:00:03 AM
Last modification on : Friday, April 5, 2019 - 8:17:36 PM

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Bastien Linol, Maarten de Wit, François Guillocheau, Olivier Dauteuil, Cécile Robin. Multiphase Phanerozoic Subsidence and Uplift History Recorded in the Congo Basin: A Complex Successor Basin. Maarten J. de Wit, François Guillocheau, Michiel C.J. de Wit (Eds.). Geology and Resource Potential of the Congo Basin, Springer, pp.213-227, 2015, Regional Geology Reviews, 978-3-642-29481-5. ⟨10.1007/978-3-642-29482-2_11⟩. ⟨insu-01116954⟩

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