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Fig. 5. | Earth, Planets and Space

Fig. 5.

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

Fig. 5.

One-dimensional velocity structures (J. Oikawa, personal communication on 12 July, 2012) used for calculating slowness values to estimate the depths of the explosion and tremor sources. The velocity structure is based on P wave velocity structures (Tsutui et al., 1996; Nishi and Kagiyama, 2002). A Poisson’s ratio of 0.25 is assumed.

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