Fig. 11.From: Continuous long-term array analysis of seismic records observed during the 2011 Shinmoedake eruption activity of Kirishima volcano, southwest JapanHorizontal and vertical cross-sections of the likelihood distribution for the source location of the continuous tremor. Graphical details are the same as in Fig. 10. The S wave apparent slowness and back azimuth were assumed to be 0.4 s/km and 265°, respectively, for likelihood calculations. The standard error for the observed slowness was assumed to be 0.08 s/km.Back to article page