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Geochronology of sedimentary and metasedimentary Precambrian rocks of the West African craton

Identifieur interne : 000518 ( France/Analysis ); précédent : 000517; suivant : 000519

Geochronology of sedimentary and metasedimentary Precambrian rocks of the West African craton

Auteurs : Norbert Clauer [France] ; Renaud Caby [France] ; Daniel Jeannette [France] ; Roland Trompette [France, Brésil]

Source :

RBID : ISTEX:63F1CA944A686D63BFC59053A5080CBB227E39F0

Abstract

This contribution summarizes current knowledge of the geochronology of the Upper Proterozoic sedimentary rocks covering the West African craton. This was done by using direct dating methods. Correlations between the northern edge of the Tindouf basin and the northern and southern part of the Taoudeni basin, as well as the Volta basin, are proposed. An important depositional lack over almost the entire craton is confirmed between 1.7 Ga, which represents the time of the latest Eburnean activities or cooling effects, and about 1.0 Ga which is the start of the general Upper Proterozoic sedimentation. This lack is remarkable as the other cratons from Gondwana continent are covered by Middle Proterozoic sediments. The Upper Proterozoic sedimentation on the West African craton may be divided into a basal, mainly sandstone period (ca. 1000-900 Ma), a middle, mainly limestone period (ca. 900-750 Ma) and an upper, mainly siltstone period (ca. 750-650 Ma). Tectonic, volcanic and thermal activities in connection with the Pan-African orogeny are recorded only around the craton. They induced either sedimentation lacks in Morocco or sedimentation excesses in Hoggar. Unsolved problems such as the precise stratigraphic position of the uppermost Proterozoic tillitic episode and the correlation within the Moroccan Anti-Atlas are also raised.

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DOI: 10.1016/0301-9268(82)90036-5


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ISTEX:63F1CA944A686D63BFC59053A5080CBB227E39F0

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<div type="abstract" xml:lang="en">This contribution summarizes current knowledge of the geochronology of the Upper Proterozoic sedimentary rocks covering the West African craton. This was done by using direct dating methods. Correlations between the northern edge of the Tindouf basin and the northern and southern part of the Taoudeni basin, as well as the Volta basin, are proposed. An important depositional lack over almost the entire craton is confirmed between 1.7 Ga, which represents the time of the latest Eburnean activities or cooling effects, and about 1.0 Ga which is the start of the general Upper Proterozoic sedimentation. This lack is remarkable as the other cratons from Gondwana continent are covered by Middle Proterozoic sediments. The Upper Proterozoic sedimentation on the West African craton may be divided into a basal, mainly sandstone period (ca. 1000-900 Ma), a middle, mainly limestone period (ca. 900-750 Ma) and an upper, mainly siltstone period (ca. 750-650 Ma). Tectonic, volcanic and thermal activities in connection with the Pan-African orogeny are recorded only around the craton. They induced either sedimentation lacks in Morocco or sedimentation excesses in Hoggar. Unsolved problems such as the precise stratigraphic position of the uppermost Proterozoic tillitic episode and the correlation within the Moroccan Anti-Atlas are also raised.</div>
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