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Fig. 11. | Earth, Planets and Space

Fig. 11.

From: Continuous long-term array analysis of seismic records observed during the 2011 Shinmoedake eruption activity of Kirishima volcano, southwest Japan

Fig. 11.

Horizontal 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.

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