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If mixing with upper layers occurred, the top depth of the lower crust can be slightly shallower.
The negative anomaly is justified by increasing the breccias thickness or increasing the top depth to the Cretaceous unit.
The top depth for each fault model is 1.5 km, which corresponds to sub-faults 1 5.
The top depth to the upper crust is ~2 km and ~4 km for the lower crust as shown in the cross-sections (Fig. 6).
We replaced the conductors with resistive blocks at different depths and the resistive blocks were set from the top depth to the last layer of the models.
The top depth of the fault model is approximately 1.5 km; its extension to the surface corresponds to the surface trace of the Hinagu fault zone (Fig. 3b).
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The top depths are 0 km and 3.5 km beneath seafloor, for subfaults 0* and 1*, respectively.
It not only indicates the horizontal locations of boundaries according to the 0° contour line, but also estimates the top depths of buried sources calculated from the horizontal distances from 45° and 90° contour line to 0° contour line.
The subfaults are placed on the Pacific plate (Nakajima and Hasegawa 2006), and the top depths beneath seafloor are 0 and 3.5 km for shallowest (row 0) and next (row 1) subfaults (Table 1).
Additionally, the corresponding top depth of resistive blocks should be the lowest boundary of the conductive layers.
A new method of the horizontal location of boundaries and the estimates of top depth of gravity anomaly sources is presented to meet the need of the quick interpretation of potential field data.
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