Fig. 4From: Unusual low-angle normal fault earthquakes after the 2011 Tohoku-oki megathrust earthquakeMoment tensor analysis of the 2014 Fukushima-oki earthquake. Moment tensor solutions—colored based on their variance—as a function of the half-duration of the source time function (Tr) and the centroid depth. The variance-contour interval is 0.025. The figure was generated with Generic Mapping Tools (Wessel and Smith 1998)Back to article page