“…The appropriate scaling factors for the dynamic events are specified in [13,19], and actual earthquake conditions could be simulated in the centrifuge model. Two input earthquake signals were used for the shaking events, including the Hachinohe earthquake motion recorded at Tokachi Oki, Japan (16 May 1968, Magnitude 7.9), which has long-period components; and the Ofunato earthquake motion recorded at Miyagi-Ken Oki, Japan (12 June 1978, Magnitude 7.4), which has short-period components (Figure 3 [24,25]). Two input earthquake signals were used for the shaking events, including the Hachinohe earthquake motion recorded at Tokachi Oki, Japan (16 May 1968, Magnitude 7.9), which has long-period components; and the Ofunato earthquake motion recorded at Miyagi-Ken Oki, Japan (12 June 1978, Magnitude 7.4), which has short-period components (Figure 3 [24,25]).…”