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In North Africa, the Algerian margin is made of basement blocks that drifted away from the European margin, namely the Kabylia, and docked to the African continental crust in the Early Miocene. This young margin is now inverted, as dated Miocene (17 Ma) granites outcrop alongshore, evidencing kilometre‐scale exhumation since their emplacement. Age of inversion is actually unknown, although Pliocene...
L'etude paleomagnetique de la formation moscovienne (~305<space>Ma) de l'anticlinal d'Edjeleh montre l'existence de trois composantes d'aimantations. Deux d'entre elles correspondent vraisemblablement a des reaimantations d'ages Cenozoque et Permien. La troisieme, determinee aussi bien par des ChRMs que par l'analyse de cercles de reaimantation, presente un test du pli positif. Sachant que le...
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