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A number of isolated events, located about 10 km below the upper plane seismicity (e.g., cross-sections C-J of Fig. 3(b)), can also be recognized.
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The seismicity of the lower plane is much less active than that of the upper plane and is located about 10 km beneath the upper plane seismicity.
Dots and open circles indicate the locations of events within the upper plane and lower plane of the DSZ, respectively.
The upper plane of the osteotomy wedge had an angle of 15° to the horizontal plane.
In this situation, the upper plane is not parallel to the lower plane in either lean or fat dimensions.
Fig. 10 Seismicity and S-wave velocity in the crust of the Pacific slab. a S-wave velocity distribution in the crust of the Pacific slab under NE Japan on a curved plane 5 km below the upper plate surface.
2, 15, and 30 km, below the upper plate interface.
Free convection takes place at the up side of the upper plate and forced convection below the upper plate.
A similar local deepening of the upper-plane seismic belt was detected below SW Hokkaido, associated with the junction of the NE Japan and Kuril arcs (Kita et al. 2010).
Events 0 10 km below the upper plate surface are shown as blue dots, and the upper-plane seismic belt is shown in pink.
Solid line is the upper plate interface, and A denotes the upper-plane seismic belt.
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