Lithofacies and Palynofacies of the Miocene Deposits in the Paralic Basin of Tunisia (Basin of the Cap Bon and Basin of Saouaf): Reconstruction of Palaeoenvironments

Author:

Moktar Nadia Ben,Mannaï-Tayech Beya

Publisher

Springer Nature Switzerland

Reference22 articles.

1. Abbes, C. (1983). Structural study of Jebel Touila. Northern extremity of the N-S Sidi Kralif-Nara-el Haouareb chain (p. 121). Thesis, Fac. Sc.

2. Bedir, M. (1995). Geodynamic mechanisms of basins associated with sliding corridors of the Atlas margin of Tunisia. Seismo-stratigraphy, seismo-tectonics and petroleum implications (p. 416). Ph.D. Thesis, Univ.

3. Ben Moktar, N., & Mannaï-Tayech, B. (2011). Reconstitution of the vegetation and climate during the Miocene in the Saouaf Basin (northeastern central Tunisia). Geodiversitas, 34, 445–456.

4. Ben Moktar, N., & Mannaï-Tayech, B. (2014). Palynology and sedimentology of the Miocene series in the north-east of Tunisia: The climatic and eustatic signature. Arabian Journal of Geosciences, 7, 385–396.

5. Ben Salem, H. (1992). Contribution to the knowledge of the geology of Cap Bon: Stratigraphy, tectonics and sedimentology. University Tunis.

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