GNGTS 2019 - Atti del 38° Convegno Nazionale

GNGTS 2019 S essione 3.1 573 References Aki K. and Chouet B.; 1975: Origin of coda waves: source, attenuation, and scattering effects. Journal of geophysical research, 80.23, pp. 3322-3342. Borleanu F., De Siena L., Thomas C., Popa M. and Radulian M.; 2017: Seismic scattering and absorption mapping from intermediate-depth earthquakes reveals complex tectonic interactions acting in the Vrancea region and surroundings (Romania). In: Tectonophysics 706, pp. 129-142. Calvet M., Sylvander M., Margerin L. and Villaseñor A.; 2013: Spatial variations of seismic attenuation and heterogeneity in the Pyrenees: Coda Q and peak delay time analysis. In: Tectonophysics 608, pp. 428-439. De Siena L., Amoruso A., Del Pezzo E., Wakeford Z. Castellano. M and Crescentini L.; 2017: Space-weighted seismic attenuation mapping of the aseismic source of Campi Flegrei 1983-1984 unrest . Geophysical Research Letters 44.4, pp. 1740-1748. Del Pezzo E., Ibanez J., Prudencio J., Bianco F. and De Siena L.; 2016: Absorption and scattering 2-D volcano images from numerically calculated space-weighting functions . In: Geophysical Journal International 206.2, pp. 742-756. Mayor J., Calvet M., Margerin L., Vanderhaeghe O. and Traversa P.; 2016: Crustal structure of the Alps as seen by attenuation tomography . In: Earth and Planetary Science Letters 439, pp. 71-80. Wortel MJR. and Spakman W; 2000: Subduction and slab detachment in the Mediterranean-Carpathian region . In: Science 290.5498 (2000), pp. 1910–1917. Fig. 3 - Q c –1 maps in the frequency bands 0.4-0.8 Hz (left) and 0.8-1.2 Hz (right).