By Walker D.E., et al. (eds.)
Computational lexicography is a fast-growing box with implications for quite a lot of disciplines--theoretical linguistics, computational linguistics, cognitive technology and synthetic intelligence--as good as for the development of dictionaries. those papers offer a baseline and a reference aspect for additional learn on difficulties linked to the lexicon. in line with the groundbreaking Grosetto Workshop, the gathering addresses many matters which are nonetheless debated at the present time and that advisor present examine and improvement
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Géol. 559-568. Guiraud, R. C. (1991). Le rifting au Crétacé inférieur: synthèse structurale, mise en évidence de deux étapes dans la genèse des bassins, relations avec les couvertures océaniques péri-africaines. Bull. Soc. Géol. 811– 823. Guiraud, R. C. (1992). Early Cretaceous rifts of western and central Africa: an overview. 153–168. ; Thierry, J. & Delplanque, A. (2005). Phanerozoic geological evolution of Northern and Central Africa: an overview. J. African Earth Sci. 83–143. , (1999). Halokinesis and structural evolution of the major features in eastern and southern Atlas.
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. Soc. Géol. 797-810. ; Amrhar, M. & Ait Ouali, R. (2002). The Mesozoic-Cenozoic Atlas belt (North Africa): an overview. 185-208. Rabhi, M. & Ben Ayed, N. (1990). Mise en évidence d’une tectonique compressive d’âge Aptien supérieur en Tunisie centrale.
The compressive deformation phases appear strongly controlled by the pre-existing geometries: folds, faults and strike-slip faults are directly induced by the paleostructures orientation of the TB. Tunisian Transtensive Basins in Tethyan Geodynamic Context and Their Post-Tortonian Inversion 41 Fig. 11. Tectonic control of compressive structures by inherited structure On the boundaries, the tectonic reactivation affects essentially vertical accidents (localized at the block limit) inducing with ancient sedimentary wedges a very superficial overthrust (Fig.
