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Figure 4 | Earth, Planets and Space

Figure 4

From: Seismic attenuation beneath Kanto, Japan: evidence for high attenuation in the serpentinized subducting mantle

Figure 4

Results of the checkerboard resolution test. The depth of each layer is shown at the upper-left corner of each panel. The black line shown at depths of 50 to 80 km denotes the iso-depth contour for the Pacific slab at each corresponding depth. Two panels in the bottom right show the results for layers in the subducting Pacific plate (where distance is measured from the slab surface).

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