Titlebook: Geological Evolution of the Mediterranean Basin; Raimondo Selli Comme Daniel Jean Stanley,Forese-Carlo Wezel Book 1985 Springer-Verlag New

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https://doi.org/10.1007/978-3-662-28948-8ve played a major role in shaping the Eastern Mediterranean. The first one, the Pelusium system, composed of the Dead Sea, Pelusium Line, and Qattara-Eratosthenes shears, is primarily responsible for the structure of the eastern Levantine Basin and the Levant. The other one, composed of the Pliny-Si

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https://doi.org/10.1007/978-3-0348-4168-9rrhenian volcanic belt, i.e., from southern Tuscany to Latium and Campania on the Apennine coastal range, Aeolian Islands, Ustica, Etna, and Sardinia. Discrepancies exist as to the origin of these fluids. Most authors suggest that the metasomatizing fluids originate from dehydration of a subducted l

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Erratum to: Die Tanninfarbstoffe,curred since the Neogene. This evolution supports the model of Messinian shallow-water evaporation within a shallow basin setting. Sedimentary facies indicate a direct relation between Messinian sedimentation and rate of basin subsidence, the latter calculated at about 1 m/1000 years. The general pa

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