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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Geophysics and Geodynamic Implications for the Evolution of the Hellenidesappears that the continental crust has been stretched considerably and thinned to about half its original thickness. The direction of expansion is north-south and northwest-southeast. In contrast to the Aegean Sea where tensional tectonics prevail, the outer Hellenic zones are structurally in a phas

flavonoids

Slice Tectonics in the Eastern Mediterranean Basinve 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

DUCE

Neogene and Quaternary Mediterranean Volcanism: The Tyrrhenian Examplerrhenian 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

interlude

Plio-Quaternary Sedimentation and Tectonics in the Ionian Area: Clues to the Recent Evolution of thecurred 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

MEAN

Models of Upper Miocene Evaporite Genesis in the Mediterranean Regionevaporite basins, such as the barred basin with one-way flow, the deep-water, wind-driven up welling, sebkha, or broad saturation shelf models, appears to be applicable to these Mediterranean evaporite cycles nor, for that matter, a model of a desiccating deep basin. Taking into account several acce

GIDDY

habile

Book 1985e biology, and ecology and man‘s influence on the natural Medi­ terranean regime. At a conference held in Banyuls-sur-Mer, France, in August 1979, Profes­ sor Raimondo Selli was urged by some panel members to initiate an Ad­ vanced Research Institute (ARI) that would focus primarily on the geologi­

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phy, marine biology, and ecology and man‘s influence on the natural Medi­ terranean regime. At a conference held in Banyuls-sur-Mer, France, in August 1979, Profes­ sor Raimondo Selli was urged by some panel members to initiate an Ad­ vanced Research Institute (ARI) that would focus primarily on the geologi­ 978-1-4613-8574-5978-1-4613-8572-1

Estimable

Aspects of the Late Cenozoic Evolution of the Aegean Region

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https://doi.org/10.1007/978-3-662-28948-8ill moderately rises and thins toward the west; excessive sediment accumulation has taken place in these troughs since Paleozoic or even late Precambrian time. The Levantine Basin, with its 15–16 km thick sedimentary sequence, is therefore considered a relict of the Tethys Ocean, which is of an appr