GNGTS 2013 - Atti del 32° Convegno Nazionale

Eberhart-Phillips D.; 1986: Three-dimensional velocity structure in Northern California Coast ranges from inversion of local earthquake arrival times . Bull. seism. Soc. Am., 76 , 1025-1052. Eberhart-Phillips D.; 1993: Local earthquake tomography: Earthquake source regions . in Seismic Tomography: Theory and Practice, edited by H.M. Iyer and K. Hirahara, Chapman and Hall, New York, pp. 613-643. Eberhart-Phillips D., Reyners M., Chadwick M. and Chiu J.; 2005: Crustal heterogeneity and subduction processes: 3-D Vp, Vp/Vs and Q in the southern North Island, New Zealand . Geophys. J. Int., 162 , 270-288. Evans J.R., Eberhart-Phillips D. and Thurber C.H.; 1994: User’s manual for SIMULPS12 for imaging Vp and Vp/Vs :A derivative of the “Thurber” tomographic inversion SIMUL3 for local earthquakes and explosions . U.S.G.S., Open File Report, 94-931, 101 pp. Franceschina G., Kravanja S. & Bressan G.; 2006: Source parameters and scaling relationships in the Friuli-Venezia Giulia (Northeastern Italy) region . Phys. Earth planet. Inter., 154 , 148-167. Gentile G.F., Bressan G., Burlini L. and De Franco R.; 2000: Three-dimensional VP and VP/VS models of the upper crust in the Friuli area (northeastern Italy). Geophys. J. Int., 141 , 457-478 Gentili S. and Bressan G.; 2008: The partitioning of radiated energy and the largest aftershock of seismic sequences occurred in the northeastern Italy and western Slovenia . J. Seismol., 12 , 343-354. Gentili S. and Franceschina G.; 2011: High frequency attenuation of shear waves in the southeastern Alps and northern Dinarides . Geophys. J. Int., 185 , 3, 1393-1416. Goldberg, D.E. Genetic Algorithms in Search, Optimization, and Machine Learning , Addison-Wesley Publishing Company, INC.,1989, ISBN 0-201-15767-5. Gruppo di lavoro CPTI, 2004. Catalogo Parametrico dei Terremoti Italiani, versione 2004 (CPTI04), INGV, Bologna, http://emidius.mi.ingv.it/CPTI04/. Haberland C., Rietbrock A.; 2001: Attenuation tomography in the western central Andes: A detailed insight into the structure of a magmatic arc. J. Geophys. Res., 106 , B6, 11151-11167. Hough S.E. and Anderson J.G.; 1988: High frequency spectra observed at Anza, California: implications for Q structure . Bull. seism. Soc. Am., 78 , 692-707. Malagnini L., Akinci A., Herrmann R. B., Pino N.A. and Scognamiglio L.; 2002: Characteristics of the ground notion in Northeastern Italy . Bull. seism. Soc. Am., 92 , 2186-2204. Mantovani E., Albarello D.,Tamburelli C. and Babbucci D.; 1996: Evolution of the Tyrrhenian basin and surrounding regions as a result of the Africa-Eurasia convergence . J. Geodyn., 21 , 35-72. Michelini A. and McEvilly T.V.; 1991: Seismological studies at Parkfield. Simultaneous inversion for velocity structure and hypocenters using cubic B-splines parametrization . Bull. seism. Soc. Am., 81 , 2, 524-552. Olsen K.B., Day S. M. and Bradley C.R.; 2003: Estimation of Q for Long-Period (>2 sec) Waves in the Los Angeles Basin. Bull. seism. Soc. Am., 93 , 2, 627-638. Oppenheim A.V. and Schafer R.W.; 1999: Discrete-Time Signal Processing . Prentice-Hall, Upper Saddle River, NJ. Rietbrock A.; 2001: P wave attenuation structure in the fault area of the 1995 Kobe earthquake , J. Geophys. Res., 106 , 4141-4154. Thurber C.H.; 1993: Local earthquake tomography: velocities and Vp/Vs – theory , in Seismic Tomography – Theory and Practice, pp. 563-583, eds Iyier, H.M. & Hirahara, K., Chapman and Hall, London. Thurber C.H., Eberhart-Phillips D.; 1999: Local earthquake tomography with flexible gridding . Computer and Geosciences, 25 , 809-818. Active deformation across the Zagros collisional belt as deduced fromgeodeticand seismological observations: preliminary results P. Imprescia 1 , M. Palano 2 , A. Agnon 3 , S. Gresta 4,5 1 Istituto di Geologia Ambientale e Geoingegneria, Consiglio Nazionale delle Ricerche, Rome, Italy 2 Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Catania, Italy 3 Institute of Earth Sciences, Hebrew University of Jerusalem, Israel 4 Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Università degli Studi di Catania, Italy 5 Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy Introduction. The current tectonic setting of the Bitlis-Zagros Fold and Thrust Belt (BZFTB) is related to the complex convergent process between the Arabian and Eurasian plates which has been continuous since Late Cretaceous times after the closure of the Neo-Tethys Ocean, with a late episode of accentuated shortening during the Pliocene-Quaternary (e.g. Dewey et al. , 1973; Numan, 1997; Abdulnaby et al. , 2013). BZFTB is ca. 1200 km long and trends NW-SE between eastern Turkey, where it connects to the Anatolian mountain belt, and the Strait of Hormuz, where it connects to the Makran subduction zone (Fig. 1). It shows two main trends: the Bitlis EW trend, between the Arabian Plate and the Anatolian tectonic block, and the Zagros NW-SE trend, between the Arabian Plate and the Iranian tectonic block (Fig. 1). 75 GNGTS 2013 S essione 1.1