Polyphasic evolution of the Jeffara basin in southern Tunisia, influence of halokinesis on the passive margin structuration in the Mesozoic and the Cenozoic

Author:

Khouni Radhouane,Arfaoui Mohamed Sabri,Dridi Soufiane,Zargouni Fouad

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference132 articles.

1. Abdeljaouad S (1987) Sur l'âge Paléocène supérieur- Miocène des dépôts continentaux a calcrètes ou dolocrètes de la formation Bou-Loufa en Tunisie méridionale. Conséquences paléogéographiques. - Bull Soc Géol Fr, Paris, (8), III, 4, pp 777-781

2. Aissaoui N, Acheche MH, Ben Yacoub J, M’Rabet A, Nehdi T, Pezzino F, Smaoui J (1996) Silurian Acacus new play in southern Tunisia. Proceedings of the 5th Tunisian Petroleum Exploration Conference, Tunis. Enterprise Tunisienne d’Activités Petroliéres (ETAP) Memoirs, 10, 1–14

3. Amor H (1999) Halokinesis and structural evolution of the major features in eastern and southern Tunisian atlas. Tectonophysics 306(1):79–95

4. Argnani A (1990) The Strait of Sicily Rift Zone: Foreland deformation related to the evolution of a back-arc basin. J Geodynum 12:315–337

5. Arthaud F, Matte P (1977) Late Paleozoic strike-slip faulting Southern Europe and Nothern Africa result of a right-lateral shear zone between the Appalachian and the Ourals. Bull. Geol. Soc. Am. 88:1305–1320

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