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(a) 3-D view of Moho depth.
However, Fig. 2(c) shows also a smooth model of Moho for the area.
The main data source for geometry of boundaries (for example, of Moho boundary) comes from seismic studies.
Table 1 Statistics of Moho depths and their differences, Sjöberg's direct solution, the Moho recovered from GOCE data (TGOCE) and the seismic Moho (TCRUST2.0).
According to Figs. 2(a) and 2(b), a smoother model of Moho is recovered from the GOCE data than that obtained from the terrestrial gravimetric data.
Fig. 2. Velocity Model for the Denizli Graben System, the depth of Moho is 29 km (modified from Akyol et al., 2006).
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Although this avoids the contamination of secondary arrivals because of the existence of the Moho, lots of good data are discarded and, as a result, the lower crust is particularly poorly constrained.
Our starting models are based on the structure of the Cascadia subduction system in Oregon in which the depth of the Moho east of the serpentinite forearc mantle wedge is about 30 km.
The modeling of the Moho in terms of the thin plate flexure model is done by a least squares approximation of the Moho obtained from gravity inversion.
These cases make up c. 6% only of the total profile length studied, confirming the interpretation of the Moho generally representing the top of the mantle.
However, the depth of the Philippine Sea slab is almost similar to that of the Moho boundary beneath the faults of Nobi earthquake (Nakajima et al. 2015).
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