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The black, green and blues contours represent slip, its error, and depth of the plate interface.
The black, green and blues contours represent slip, its confidence interval and depth of the plate interface.
Seismic structure at the depth of the plate interface provides important information for understanding the occurrence of interplate earthquakes.
The depth of the plate interface is indicated as contours with an interval of 20 km (Miyazaki et al. 2004).
The black, green and blue contours represent slip, standard deviation of slip and depth of the plate interface.
However, it should be emphasized that low-angle normal fault earthquakes at approximately the depth of the plate interface are unusual in subduction zones.
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To the north, several thrust-faulting earthquakes with shallowly dipping nodal planes are located over a range of depths less than 40 km, while the depth to the plate interface below their epicenters is ~50 km.
To the east of the 20 km depth contour of the plate interface, ΔCFF first takes a negative value between the 10 and 20 km depth contours, and then takes a positive value beyond the 10 km depth contour toward the trench.
The area west of the 20 km depth contour of the plate interface is dominated by a positive ΔCFF.
Dashed lines show depth contours of the plate interface (Noguchi, 1996; Nakamura et al., 1997).
The boundary of the positive and negative lobes coincides with the 20 km depth contour of the plate interface.
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