DOI: 10.1016/J.SOILDYN.2016.09.006
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摘要: Abstract This paper examines the salient characteristics of near-source strong ground motions recorded from 13 June 2011 Mw6.0 Christchurch, New Zealand earthquake. 26 were within Rrup=30 km source, with maximum geometric mean horizontal shaking exceeding peak accelerations and velocities PGA=1.5 g PGV=100 cm/s, respectively. The polarity motion recordings with Rrup