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/10.1007/978-3-322-99087-7h to trigger the type of motion suggested by some workers. It is envisioned that the present-day deformation of the Aegean is a response to vertical movement of lithothermal masses rather than to horizontal deformation and subduction.

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Geophysics and Geodynamic Implications for the Evolution of the Hellenidesh to trigger the type of motion suggested by some workers. It is envisioned that the present-day deformation of the Aegean is a response to vertical movement of lithothermal masses rather than to horizontal deformation and subduction.

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Book 1985 intricate pieces, many of which are already in place. A general image, in terms of science, has emerged, although at this time large gaps are noted and some areas of the picture remain fuzzy and indistinct. In recent years this fascinating, mind-teasing puzzle image has become clearer with individu

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Geological Information from Satellite Surveys of the Mediterranean Regionns for a given region, but it is necessary to “field check” any area for which lineament maps are prepared. It is critical that such studies be carried out within known morphotectonic regions or smaller domains in which geologic parameters are similar.

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Seismicity of the Mediterranean Basinan and the closing of the Mediterranean Sea. Main tectonic features are of compressive character, with only very localized zones undergoing horizontal tension. The oceanic crust of the Mediterranean Basin is divided into two parts by the Italian peninsula, with the western part belonging to the Eurasian plate and the eastern to the African plate.

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Tectonic Evolution of the Tyrrhenian Seail the present a process of oceanization by mantle diapirism took place in the Tyrrhenian area associated with an extensional tectonic regime oriented east-west. The consequent isostatic foundering produced the Tyrrhenian Sea and governed its progressive deepening.

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https://doi.org/10.1007/978-3-662-41335-7Extension of the crystalline basement away from the coasts can be followed by DRS and aeromagnetism. The crust-to-mantle transition is not always evident, and can be a progressive one; prevailing tension fractured the crust and fostered magmatic intrusions and effusions as revealed by magnetic anomalies.

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https://doi.org/10.1007/978-3-642-92281-7ian Basin. Such kinematics and chronology are consistent with pa-leomagnetic data supporting the Sardinian rotation, basin and margin structure, subsidence since 21 m.y, (especially during Messinian time), and heat flow measurements.

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,Orientierung über die Elektronentheorie,ont) foreland basements, respectively. The eastern, seismically active front is believed to have resulted from a process of Neogene Apenninization of the previous Alpine fold structures, triggered by the eastward migration of domal uplifts, transient in time and space.