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Additional resources for New Frontiers in Tectonic Research - At the Midst of Plate Convergence
Eds), Encyclopedia of Geomagnetism and Paleomagnetism, Springer, 475-477. A. (1967). AC demagnetization of rocks: analysis of results. K. ), Method in Paleomagnetism. Elsevier, Amsterdam, 254–286. 2 Tunisian Transtensive Basins in Tethyan Geodynamic Context and Their Post-Tortonian Inversion 1University Adel Rigane1 and Claude Gourmelen2 of Sfax-Tunisia, Faculty of Sciences, Department of Geology, RU: GEOGLOB (03/UR/10-02) 2University of Maine, Faculty of Sciences, Geosciences Laboratory 1Tunisia 2France 1.
1989), intersected by local depocentres associated with grabens or hemi-graben structures linked to the regional extension and arranged according to transverse faults following the axial trend. , 1999; Soussi, 2002) combined with the existing tectonics allows us to propose a simple geometrical model of the Tunisian basin at that time: three unstable zones are arranged around a resistant central block with little or no subsidence, and are subject to the remobilization of pre-Triassic basement fractures.
Rouvier, H. (1977). Géologie de l’extrême nord tunisien : tectoniques et paléogéographie superposées à l’extrémité orientale de la chaîne nord maghrébine. Thèse d’Etat, Université Paris-VI, 898 p. Schettino, A. & Scotese, C. (2002). Global kinematic constraints to the tectonic history of the Mediterranean region and surrounding areas during the Jurassic and Cretaceous. In: In: Rosenbaum, G. and Lister, G. S. 2002. Reconstruction of the evolution of the Alpine-Himalayan Orogen. 148-168 Soussi, M.