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La marge africaine du canal du Mozambique, le système turbiditique du Zambèze : une approche « Source to Sink » au Méso – Cénozoïque

Abstract : The Zambezi system located on the eastern slope of Africa is characterized by a turbiditic system of very large size (x 100 km) and is associated onshore to the third largest watershed in Africa (1,320,000 km2) after those of the Nile and Congo. Few studies have examined the evolution of the land - sea system from the eroding catchment to the sedimentation basin. This work will focus on: [1] characterize and discuss the origin of the deformations recorded in the Zambezi sedimentary system since 155 Ma, [2] quantify the erosion-sedimentation balances of the Zambezi system, for a better understanding of the sedimentary routing
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https://tel.archives-ouvertes.fr/tel-01865479
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Submitted on : Friday, August 31, 2018 - 3:44:18 PM
Last modification on : Wednesday, September 9, 2020 - 4:52:52 AM
Long-term archiving on: : Saturday, December 1, 2018 - 3:55:42 PM

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  • HAL Id : tel-01865479, version 1

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Jean-Pierre Ponte. La marge africaine du canal du Mozambique, le système turbiditique du Zambèze : une approche « Source to Sink » au Méso – Cénozoïque. Sciences de la Terre. Université Rennes 1, 2018. Français. ⟨NNT : 2018REN1B005⟩. ⟨tel-01865479⟩

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