“…1 Hz GPS recordings have been used to detect motions of the Earth's surface associated with seismic-wave propagation Houlié et al, 2011;Kaloop and Rabah, 2016), for earthquake early warning (Allen and Ziv, 2011;Bock et al, 2011), to invert for coseismic slip of large (M w > 6) events (Miyazaki et al, 2004;Miyazaki and Larson, 2008;Rhie et al, 2009;Houlié et al, 2014), to constrain seismic moment magnitude (Melgar et al, 2015), and to record the Earth's normal modes (Mitsui and Heki, 2012), or simply coseismic offsets . Psimoulis et al (2014) showed that it is possible to establish maximum ground velocity (MGV) maps at long periods (T > 3 s) using high sampling rate GPS data collected during the 2011 Tohoku-Oki megathrust event. Some deep basins in Japan with a fundamental period of 3 s or more showed large amplifications of the long-period ground motion during the Tohoku-Oki event, which are not taken into account by commonly used high-frequency amplification proxies such as V S30 .…”