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The onset time of this velocity reduction suggests that the velocity reduction is likely associated with the M 5.7 Greenville earthquake (Fig. 7a).
The maximum velocity reduction is ~ 60 m/s (~ 4%) at level 2 (Panel B).
Our monitoring system identifies a sudden velocity reduction of ~0.1 % in a depth of 1 km.
After this velocity reduction, the dv/v gradually increased over time.
We searched for local and teleseismic earthquakes that might be linked to this velocity reduction.
The velocity reduction started immediately after the onset of the tilt change and the swarm activity.
Velocity reduction is carried out in the pump casing by recuperators.
Furthermore, the velocity reduction ratio is inversely proportional to the spacing between adjacent rows.
Our results show an overall change of the velocity reduction from east to west in this region (Fig. 8), with the strongest velocity reduction (~8.5%) in the eastern part (near the northwestern edge of African Anomaly).
Fig. 7 a Coseismic velocity reduction associated with the 24 May 2013 M 5.7 Greenville earthquake (dashed red line).
A velocity reduction of up to −1.06 % was observed within 10 days after the occurrence of the Tohoku-oki earthquake.
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