Establishment of the stratigraphy of the Tell (Maritime) Atlas range in Algeria reveals structural anomalies, principally a structural depression crossing the entire Tell region and folds and faults oblique to the general east-west trend of the region. These are explained as the result of major dislocations of the basement, which have a northeast-southwest orientation. It is suggested that similar anomalies in other parts of Algeria can be explained on the same basis.

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