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Fig. 10 | Earth, Planets and Space

Fig. 10

From: Combined approach to estimate the depth of the magma surface in a shallow conduit at Aso volcano, Japan

Fig. 10

Example waveforms of seismo-acoustic signals. These waveforms have a a short time delay and b a long time delay of the arrivals. Dashed lines are the arrival times read manually. The solid line shows the time 1.12 s before the infrasound arrival. The maximum value of the time delay that can be reproduced by our model is 1.12 s. However, the time delay of example b seems to be longer than 1.12 s. Perhaps the initial phase of the infrasound signal was not excited well, causing the time delay to appear to be extended

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