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Exact(2)
where γ is the gravitational constant and Δρ is the density contrast between the sedimentary layer and basement.
As shown in Fig. 2, an average boundary depth between the sedimentary layer and basement is defined as z = D (>0).
Similar(58)
In the same way as described by Hino et al. (2000), we estimated the time delays due to the sedimentary layer from the arrival-time differences (T ps ) between the direct P- and S-waves converted from the direct P-wave at the base of the sedimentary layer.
Purple areas show the sedimentary layer on the Sagami Knoll.
The base of the sedimentary layer is defined down to the top of the volcanics layer, and coal layer(s) intermittently reside within the sedimentary layer.
b Sedimentary basin model where the sedimentary layer is in contact with the basement by reverse faults of 45° dip.
The sedimentary layer which consists of three layers is present throughout the entire.
Due to uncertainty of the thickness of the sedimentary layer and seismic velocity in the sedimentary layer, we used the following method.
Orange, green, and black areas show the sedimentary layer of the Sagami Trough.
At first, we introduced the sedimentary layer thickness constrained by the SCS data.
The seismic visibility of the fault zone depends on the contrasts between the porosity and the fracturation density of the sedimentary layers.
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