Dutykh, Denys; Dias, Frédéric - In: Mathematics and Computers in Simulation (MATCOM) 80 (2009) 4, pp. 837-848
In classical tsunami-generation techniques, one neglects the dynamic sea bed displacement resulting from fracturing of a seismic fault. The present study takes into account these dynamic effects. Earth’s crust is assumed to be a Kelvin–Voigt material. The seismic source is assumed to be a...