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1971) suggest that the sediments are 5-6 km thick. 4 kmJsec Vp ), 5 km thick. 5 km thick. 2 km of deformed salt. The pre-evaporite formation should be about 3-4 km thick, above a non-sedimentary crust. Finetti and Morelli (1973, p. , Fig. 8 km thick locally (WA-6). Drilling on the edge of the abyssal plain west of Sardinia (Site 134) in 1970 penetrated only the top of the Mediterranean evaporite. Later, at Site 372 south of Minorca, the drill passed through the evaporite and penetrated hemipelagic formations of Miocene age below.

65, p. 107-118. , 1970, Etude petrographique des ophiolites et des granites du flysch des Gets (Haute-Savoie, France), Arch. Sci. (Geneve), V. 23, p. 279-542. , 1972, Fission track ages of gabbro from northern Apennines ophiolites, Earth Planet. Sci. , v. 14, p. 242-244. , Mugniot, J. , 1974, Geology of the Mediterranean sea basins, in: The Geology of Continental Margins Burk, C. , and Drake, C. , New York: Springer-Verlag, p. 695-721. Bishop, W. , 1975, Geology of Tunisia and adjacent parts of Algeria and Libya, Amer.

Geol. , v. (7) 8, p. 1014-1017. Meulenkamp, J. , 1969, Stratigraphy of Neogene deposits in the Rethymnon Province, Crete, with special reference to the phylogeny of uniserial Uvigerina from the Mediterranean region, Utrecht Micropal. , v. 2, p. 1-108. , 1974, Le domaine d'Antalya, temoin de la fracturation de la plateforme africaine au cours du Trias, Soc. Geol. , v. (7) 16, p. 116-127. Moores, E. , 1969, Petrology and structure of the Vourinos ophiolite complex, northern Greece, Geol. Soc. Amer.

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