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Figure 4 | Earth, Planets and Space

Figure 4

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 4

Normalized RMS envelopes of the filtered vertical velocity seismograms. The time was measured from the arrival of the P wave. The isodepth lines in the map are the same as in Figure 1a. The averaged epicentral distances of stations N.OOKH, N.ENZH, N.NSHH, and N.HYNH are 96, 103, 111, and 155 km, respectively.

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