Fig. 3.From: Shear-wave splitting in a region with newly-activated seismicity after the 2011 Tohoku earthquakeExamples of waveforms recorded at two stations (A and B). Waveforms with N-S and E-W components are shown in (a), with maximum cross-correlation waveforms shown in (c). Original and anisotropy-corrected particle motions are shown in (b) and (d), respectively.Back to article page