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The Moroccan Anti-Atlas: the West African craton passive margin with limited Pan-African activity. Implications for the northern limit of the craton

✍ Scribed by El Hafid Bouougri

Book ID
117461779
Publisher
Elsevier Science
Year
2003
Tongue
English
Weight
85 KB
Volume
120
Category
Article
ISSN
0301-9268

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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)