GNGTS 2014 - Atti del 33° Convegno Nazionale

emitting Earth view. A simplistic evaluation of the regime of the convective motion in the mantle and of the order of magnitude of the involved forces (viscous, buoyancy, inertial) hastily judges as negligible the role of the Coriolis effect in producing the observed slope differences of the Wadati-Benioff regions. References Bacon F.; 1620: Novum Organum, sive Indicia Vera, de Interpretatione Naturae. Italian translation and introduction by Enrico De Mas, 1968. Laterza, Bari, 283 pp. Barnett C.H.; 1969: Oceanic rises in relation to the expanding Earth hypothesis. Nature, 221 (5185), 1043-1044. Bianco G.; 2005: Gli effetti del terremoto del sud-est asiatico sulla geodinamica globale. PowerPoint file of the seminar held at the Meeting “Il Terremoto-Maremoto nel Sud-Est Asiatico del 26 dicembre 2004”. Accademia Nazionale dei Lincei, Roma January 25, 2005, http://www.fis.uniroma3.it/ plastino/ seminars/terr_mar.html Bostrom R.C.; 1971: Westward displacement of the lithosphere. 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Isacks B.L., Barazangi, M.; 1977: Geometry of Benioff zones: lateral segmentation and downward bending of the sub- ducted lithosphere. In: M. Talwani and W.C. Pitman (eds.) Island Arcs, Deep Sea Trenches, and Back-arc Basins. Maurice Ewing Series I, Amer. Geophys. Union, 99-114. 180 GNGTS 2014 S essione 1.2

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