Abstract
We infer temporal changes in the elastic properties of the edifice
of Merapi volcano (Java, Indonesia) before its eruption in 1998 by
analyzing multiply scattered elastic waves excited by a repeatable
controlled seismic source. A pre-eruptive increase of shear wave
velocity, which correlates well with pre-eruptive seismicity and
dome-growth is revealed. The method can be used as a 'pressure-gauge'
for pressure changes inside of volcanoes, because increasing pressures
in rocks are known to cause proportionally increasing elastic wave
velocities.
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