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

怒目而視

Deep structure from seismic tomography,mechanisms has been ongoing for many years. One of the reasons for this has been the poor knowledge of the crust and upper mantle structure, and the lack of precise information on the occurrence of intermediate and deep earthquakes beneath the Italian peninsula. In this chapter we describe the advan

上坡

geometrician

Water-Brash

Volcanism in the Southern Apennines and Sicily,any to Basilicata, which includes the Alban Hills south of Rome, Vesuvius, the Campi Flegrei caldera, and the isolated Mt Vulture volcano; (2) the Tyrrhenian oceanic basin; (3) the Aeolian island arc; (4) eastern Sicily with Etna and the Hyblean plateau; and (5) the submarine and emerged volcanoes i

CRAFT

Basement and early (pre-Alpine) history,rly expressed by the transition from the Quaternary SE Tyrrhenian oceanic crust to the possible late Proterozoic age of the Panafrican consolidated NE Apulian continental crust (Vai, 1994), which occurs in over a distance of only 170 km. Between the two, several other crustal provinces are found in

FER

Ophiolites, Ligurides and the tectonic evolution from spreading to convergence of a Mesozoic Westerde unique records for reconstructing the opening, evolution and closure of the portion of Western Tethys that separated the European-Iberia plates to the NW from the Africa-Adria plates to the SE (Abbate .., 1970, 1980, 1986; Principi and Treves, 1984). They are present all along the Alps and the Ap

Lucubrate

essential-fats

背信

Inner Northern Apennines,e and on the Tuscan metamorphic complex (Boccaletti .., 1971; Alvarez .., 1974; Kligfield, 1979). The ophiolite-bearing Ligurides derived from the southern extension of the Ligurian—Piedmont ocean, from which similar mafic components of the Western Alps also derive (Fig. 14.1). The Tuscan units deri

AMITY

Outer Northern Apennines,nding through Romagna and Umbria—Marche to northern Latium. From the SW to the NE, it is situated between the inner Northern Apennines and the Po Plain—Adriatic foreland. To the S, the volcanic products of the Roman magmatic province cover it, while to the SE it is bounded by the Latium—Abruzzi carb