Ambient seismic noise tomography reveals a hidden caldera and its relation to the Tarutung pull-apart basin at the Sumatran Fault Zone, Indonesia
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文摘

We derived a 3D seismic velocity model by ambient noise studies at the Sumatra fault.

Surface wave phases were used to invert for S-wave structure at depth by tomography.

The model shows a velocity anomaly, interpreted as a previously unknown caldera.

It is related to numerous volcanic hot springs, potential sources of geothermal energy.

Hidden volcanic calderas represent a good indicator for geothermal prospection.

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