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Based on the interpretation of geological maps, seismic reflection and well data complemented with a bibliographic compilation and field work in the Rif, we investigate the factors that control the rift initiation, its development and the formation of oceanic crust in NW Africa. From SE to NW, we examine the Western Sahara Atlas, the Tendrara, the Guercif, and the Rif basins, to establish their geodynamic evolution in relation with the Mesozoic formation of the Central Atlantic and Maghrebian Tethys oceans, respectively. The Triassic extension was diffuse and developed over Lower Carboniferous horst-and-graben structures formed in the NW passive margin of Gondwana and involved in the subsequent late Carboniferous – early Permian Variscan orogenic system; suggesting that, at the onset of the Triassic rifting, the lithosphere was thermally re-equilibrated and replaced by more fertile lithospheric mantle. Afterwards, extension resumed in the Atlas system during middle to late Pliensbachian and finished during Toarcian. In the Rif and Guercif basins, the extension began later, mainly during the Toarcian, climaxing during Middle Jurassic times with the exhumation along low-angle extensional faults of CAMP gabbroic bodies and the final mantle exhumation during Upper Jurassic in the Rif. The study evidences the prominent role of the Variscan structural and thermal inheritance on the subsequent deformation events. Accordingly, the Paleozoic inverted basins and horsts localized the Triassic extension. From that, the opening of the Central Atlantic and Maghrebian Tethys oceans activated, respectively, the SE (Atlas) and NW (Tethys) rifted segments of the weakened continental crust where the Jurassic extension was gradually distributed. This led to the final formation of an oceanic domain in the NW paleomargin of Africa. • The tectonic/thermal features, inherited from Paleozoic events, were reactivated and controlled the subsequent Mesozoic extension in NW Africa. • Triassic extension was diffuse and developed over both former lower Paleozoic horsts and Lower Carboniferous basins in a thermally re-equilibrated lithosphere. • Jurassic far-field extensional deformations and their orientations were recorded by the NW African basins during the gradual opening of both the Central Atlantic and Maghrebian Tethys oceanic domains. [ABSTRACT FROM AUTHOR]

This article deals with the legal aspect concerning female genital mutilations (FGM). Such a practice (a partial excision of the external genitalia) is highly widespread in Central Africa, especially in Ethiopia and Somalia, and currently involves approximately 130,000,000 women worldwide and, in Italy, about 30,000 women amongst the immigrant population. Since 1982 the World Health Organization (WHO), which condemns such a practice as injurious to women's rights and health, proposed that laws and professional codes prohibit it in all countries. Legislation, although insufficient as a sole measure, is considered indispensable for the elimination of FMG. Since a long time some western countries (Sweden, Great Britain, Belgium and Norway), involved by immigration from countries with FGM tradition, legislated with regard to FGM. In Italy, a specific law does not exist; however, FGM are not allowed by the article 5 of the Civil Code. Nevertheless, recently, several cases of mutilations took place: this led some members of the Parliament to introduce a bill in order to specifically forbid FGM. The authors believe that legislation could effectively support the job of prevention and education, which physicians may carry out in order to save little girls from the risk of familial tradition of genital mutilations.