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Fig. 10 Schematic of mechanisms causing velocity reductions.
These two events showed different characteristics in their velocity reductions, implying different mechanisms.
The velocity reductions at many stations occurred rapidly in comparison with those during the 2013 activity.
In other words, the velocity reductions in region 2 more likely result from the CMB beneath southern Sumatra Islands.
We binned the P-wave velocity reductions using a 10-degree moving window with a 5-degree overlap.
Some low velocity zones with velocity reductions of 3 5% are also detected on the source side beneath southern Sumatra Islands.
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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 velocity reduction ratio increases with an increase in the density; increasing the density from 1200 to 2100 kg/m3 can lead to a 20% increase in the velocity reduction ratio.
After this velocity reduction, the dv/v gradually increased over time.
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.
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