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Finite element modelling of the recent-present deformation pattern in the Calabrian are and surrounding regions

and Eurasia. The proposed modelling approach                      ANDERSON, H. and J. JACKSON (1987): Active tectonics of
tries to simulate the presence of major tectonic                       the Adriatic region, Geophys. J. R. Astron. Soc., 91,
discontinuities - indicated by seismotectonic                         937-983.
studies - by the use of highly deformable nar-
row zones.                                                        ANTONELLI, M., R. FRANCIOSI, G. PEZZI, A. QUARCI, G.P.
                                                                       RoNCO and F. VEZZANI (1988): Paleogeographic evo-
    The kinematic boundary conditions imposed                          lution and structural setting of the northern side of
on the model are accommodated by the lateral                           Sicily Channel, in Proceedings 74th Congr. Soc. Geo!.
escape of crustal wedges in Calabria and                              ltal., 79-86.
Sicily. The resulting microplate kinematics
produces the distribution of recent-present                       ARGNANI, A. (1993): Neogene basins in the Strait of Sicily
compressional, tensional and transcurrent de-
formations observed in the study area. This                            (Centrai Mediterranean): tectonic settings and geody-
could imply that «interual» driving forces, such                       namic implications, in Recent Evolution and Seismicity
as gravitational sinking or active rifting, are                        of the Mediterranean Region, edited by E. BosCHI,
not necessary to account for extensional tec-                          E. MANTOVANI and E. MORELLI (Kluwer Academic
tonics in the Southern Tyrrhenian and Sicily                          Publishers, Dordrecht), 173-187.
Channel.                                                          ARGNANI, A., S. CORNINI, I. TORELLI and N. ZITELLINI
                                                                       (1987): Diachronous foredeep-system in the Neogene-
    The results obtained point out that the pres-                      Quatemary of the Strait of Sicily, Mem. Soc. Geo!. lt.,
ence of major tectonic discontinuities where                           38, 123-130.
strain can be much higher than in the surround-                   AVOUAC, J.P. and P. TAPPONIER (1993): K.inematic mode!
ing zones strongly affect the computed dis-                            of active deformation in Centrai Asia, Geophys. Res.
placement field. This implies that modelling                           Lett., 20 (l 0), 895-898.
approaches which neglect such tectonic fea-                       BALDI, P., V ACHILLI, F. MULARGIA and F. BROCCIO
•:ures could provide unreliable indications.                           (1983): Geodetic surveys in the Messina Straits area,
                                                                       Boli. Geod., 57, 283-293.
                 Acknowledgements                                 BARBANO, M.S., M.T. CARROZZO, P. CAVERNI, M.
                                                                       COSENTINO, G. FONTE, F. GHISETTI, G. LANZAFAME,
    We are grateful to Profs. P. Gasperini and
R. Sabadini for a criticai reading of the                              G. LOMBARDO, G. PATANÈ, M. RIUSCETTI, L. TOR-
manuscript and for fruitful suggestions. This                          TORICI and L. VEZZANI (1978): Elementi per una carta
research has been supported by the National
Research Council (CNR-GNDT), the Agenzia                               sismotettonica della Sicilia e della Calabria Meri-
Spaziale Italiana (ASI) and the Ministry of Re-                        dionale, Mem. Soc. Geo!. lt., 19, 681-688.
search and Education (MURST).                                     BARONE, A., A. FABBRI, S. ROSSI and R. SARTORI (1982):
                                                                       Geologica! structure and evolution of the marine areas
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