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Figure 3 | Earth, Planets and Space

Figure 3

From: Velocity increase in the uppermost oceanic crust of subducting Philippine Sea plate beneath the Kanto region due to dehydration inferred from high-frequency trapped P waves

Figure 3

Filtered velocity seismograms of the vertical component recorded at the N.NSHH station for all earthquakes. The time was measured from the arrival of the P wave and the amplitude was normalized to the maximum amplitude observed for the 15-s time window, starting 5 s prior to the arrival time of the P wave. The average epicentral distance of the N.NSHH station is 111 km. The isodepth lines in the map are the same as in Figure 1a.

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