Fig. 3From: Unusual low-angle normal fault earthquakes after the 2011 Tohoku-oki megathrust earthquakeP-waveform traces of the 2014 Fukushima-oki earthquake. Normalized waveform traces of the unfiltered, vertical component of P-waves as a function of station azimuth relative to the earthquake epicenter. One side of each trace is shaded. The figure was generated with Generic Mapping Tools (Wessel and Smith 1998)Back to article page