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However, the lower seismic plane is usually located at depths of several tens of kilometers, to as deep as c. 40 km, below the upper slab surface.
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Dotted and solid lines indicate the upper slab surface and the slab Moho, respectively.
P T paths for the upper slab surface and slab Moho are shown as colored solid and dot dashed lines, respectively.
Above the wall is another horizontal slab which acts as the fountain and features the same design as the upper horizontal slab.
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.
Free convection takes place at the up side of the upper plate and forced convection below the upper plate.
2, 15, and 30 km, below the upper plate interface.
Below the upper floor windows are panelled aprons and consoles.
The amount of fibres in the upper and lower slab halves has been analysed.
These were then extrapolated to the inland areas, assuming a constant difference (approximately 7 8 km) between the depth of the top of the SOC2 and the depth of the upper boundary of the slab (see below).
(4) Consequently, the upper-plane seismic belt in the Pacific slab deepens locally and is oblique to the 70 90 km depth contours of the upper surface of the slab, as shown in Fig. 7a.
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