Lithostratigraphic framework and correla
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El Hafid Bouougri; Ali Saquaque
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Article
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2004
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Elsevier Science
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English
⚖ 653 KB
The Neoproterozoic volcano-sedimentary cover (∼0.8Ga) deposited on the northern passive margin of the West African craton occurs in the central Anti-Atlas inliers and is a ∼2km thick succession formally termed the Tizi n-Taghatine Group. The group comprises two sedimentary packages (lower and upper)