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Cross-hole seismic tomography results showed low velocity (p-wave) zones around the same location corresponding to the high attenuation zone in FDAT, bringing the dormant weak zone to light.
The area of high uplift is spatially correlated with a high attenuation zone for ground penetrating radar (Yokota et al. 2008), indicating the presence of very shallow mudstone layers decomposed into soft clay with high water content.
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The FDAT clearly showed presence of anomalous high attenuation zones in the depth range of 23 33 m of the tomographic plane.
The swarm zone was imaged as high-attenuation zone.
The active seismicity can be seen on the extremely high-attenuation zone (eHAZ).
The down-warping high-attenuation zone was mapped by SAP between Miyakejima and Kozushima.
However, considering the difference in depth between the high-attenuation zone and the hypocenter distributions from OBS networks, it would be impossible that the high-attenuation zone is explained by only the 2000 swarm.
As a result, the former was imaged as low-attenuation zone, whereas the latter as high-attenuation zone.
Interestingly, a remarkable high-attenuation zone was detected between Miyakejima and Kozushima islands, being well correlated with the hypocenter distribution of the earthquake swarm in 2000.
The high-attenuation zone is interpreted as a fractured area that was developed by magma activity responsible for the earthquake swarms that have been repeatedly occurring there.
Drastic change in the average Q near the lower boundary of the high-attenuation zone caused the abnormally large interval Q values.
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