Titlebook: Anatomy of an Orogen: The Apennines and Adjacent Mediterranean Basins; Gian Battista Vai,I. Peter Martini Book 2001 Springer Science+Busin

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Geomorphologic setting,t a relatively fast rate (about 2500 m/Ma or 2.5 mm/a; Po Plain). Active tectonism renders this area prone to geological hazards such as those associated with volcanism, faulting and earthquakes, and slope instability.

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originality

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Formidable

Population Models With Constant Rates,ynamic context of Italian magmatism is discussed in much detail by Serri ... (this vol., Ch. 8), only brief summaries of the various recent hypotheses regarding the tectonic settings of these volcanoes will be given here.

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Strategies for Investment in Optionsits of the foreland consist of Mesozoic—Cenozoic carbonates up to 10 km thick (Burollet .., 1978; Patacca .., 1979; Bianchi .., 1989; Mostardini and Merlini, 1988), whereas the oceanic Ionian crust underlies thin Mesozoic—Cenozoic, deep-sea to oceanic sediments (Finetti .., 1996).

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Deep structure from seismic tomography,ological tools, exploiting this huge dataset, have helped to unravel the complex structure of the lithosphere—asthenosphere system of the Mediterranean, and, thus, have contributed to a better understanding of the geodynamic evolution of the region.

MEAN

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,The Apenninic—Maghrebian orogen in southern Italy, Sicily and adjacent areas,its of the foreland consist of Mesozoic—Cenozoic carbonates up to 10 km thick (Burollet .., 1978; Patacca .., 1979; Bianchi .., 1989; Mostardini and Merlini, 1988), whereas the oceanic Ionian crust underlies thin Mesozoic—Cenozoic, deep-sea to oceanic sediments (Finetti .., 1996).

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world. The Apennines are the place from which Steno(1669) first stated the principles of geology. The Apennines alsorepresent amongst others, the finding/testing sites of processes andproducts like volcanic eruptions, earthquakes, olistostromes andmélanges (argille scagliose), salinity crisis, geoth