New Frontiers in Tectonic Research - At the Midst of Plate by Uri Schattner

By Uri Schattner

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Géol. 145-154. Perthuisot, V. (1978). Dynamique et pétrogenèse des extrusions triasiques en Tunisie septentrionale. Thèse Doct. Ès-Sc. , Ecole Norm. , Paris, 312p. Pervinquière, L. (1903). Etude géologique de la Tunisie centrale. R. DE Rudeval. ), Thèse doct. es-sciences, Paris. 360p. ; Rekhiss, F. & Tricart, P. (1998). Evolution structurale des domaines atlasiques du Maghreb au Méso-Cénozoïque ; le rôle des structures héritées dans la déformation du domaine atlasique de l’Afrique du Nord. Bull.

Thèse Doctorat ès-Sciences. Univ. Tunis El Manar, 437p. Aissaoui, D. (1984). Les structures liées à l’accident sud-atlasique entre Biskra et le Jebel Manndra, Algérie, évolution géométrique et cinématique. Thèse 3ème cycle, Univ. L. Pasteur, Strasbourg, 145p. 44 New Frontiers in Tectonic Research - At the Midst of Plate Convergence Ben Ayed, N. (1980). Le rôle des décrochements E-W dans l’évolution structurale de l’Atlas tunisien. C. R. somm. Soc. Géol. 29-32 Ben Ayed, N. (1986). Evolution tectonique de l’avant-pays de la chaîne alpine de Tunisie du début du Mésozoïque à l’Actuel.

Elf Aquitaine Editions, Pau, 16, pp. 553-561. , Bessedik, M. P. (2008). Biostratigraphie et lithologie des séries serravallo-tortoniennes du massif du Dahra et du bassin du Chélif (Algérie). Implications sur la position de la limite serravallo-tortonienne. Geodiversitas, 30 (1). , Belkebir, L. & Mansour, B. (2002). Révision de l’âge Miocène inférieur (au sens des anciens auteurs) des dépôts du bassin du Bas Chelif (Oran, Algérie) : conséquences biostratigraphique et géodynamique. Mémoires des Services Géologiques d’Algérie, 11, pp.

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