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Figure 2 | Earth, Planets and Space

Figure 2

From: Spatial variation in coda Q around the Nobi fault zone, central Japan: relation to S-wave velocity and seismicity

Figure 2

Temporal variations in Q C -1at five frequency bands. Temporal variations in Q C -1 at frequency bands of (a) 1 to 2 Hz, (b) 2 to 4 Hz, (c) 4 to 8 Hz, (d) 8 to 16 Hz, and (e) 16 to 32 Hz. The dashed line of each panel shows the occurrence of the 2011 off the Pacific coast of Tohoku earthquake. The bars show the individual error, which is represented by the standard deviation, of Q C -1. The solid line and the hatched zone show the average and the standard deviation, respectively, of Q C -1 before and after the 2011 off the Pacific coast of Tohoku earthquake.

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