“…One of the first contributions in absorbing boundaries, but still one of the most popular ones, is the fully-local, viscous boundary element by Lysmer & Kuhlemeyer (1969). This boundary provides the conceptual basis of most of the currently used elements, which exhibit various levels of efficiency with increasing levels of nonlocality, (Berenger, 1994;Soudkhah & Pak, 2012;Lee et al, 2012;Zheng et al, 2013;Duru & Kreiss, 2012). Moreover, many of these absorbing conditions have been used in recent FDs and FEs simulations of seismic regions, as large as the state of California and for frequencies up to 4.0 Hz, (Frankel, 1993;Komatitsch & Tromp, 1999;Min et al, 2003;Bielak et al, 2003;Komatitsch et al, 2004;Givoli, 2004;Frehner et al, 2008;Ichimura et al, 2009;Lee et al, 2009aLee et al, ,b, 2010Bielak et al, 2010;Chaljub et al, 2010;Lan & Zhang, 2011).…”