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Fig. 11 Cross section of the distribution of aftershocks which occurred within the length of segment.
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A small rectangle shows the area of (a). Figure 1(b) and 1(c) shows vertical cross sections of the distribution of the similar earthquakes and the aftershocks projected on a vertical plane perpendicular to the strike.
In a cross section of the hypocentral distribution projected on a vertical plane along the seismic survey (Nakahigashi et al., in preparation), we can clearly see the relation between the aftershock distribution and the seismic velocity structure (Fig. 6).
In a vertical cross section of the hypocentral distribution, the aftershocks occurred in the plate boundary region between the subducting Pacific plate and the landward plate including the subducting oceanic crust and the 6.2-km/s layer in the overriding plate.
After demonstration the good predictive performance of the proposed analytical approach, parametric studies were carried out to analytically evaluate the influence of the main material properties, and CFRP and groove cross section on the distribution of the CFRP tensile strain and bond shear stress, and on the prestress transfer length.
Mesh boundaries are defined as parametric curves generated using trigonometrical modelling of the axial cross section of the machine while the distribution of computational nodes is performed using algebraic algorithms with transfinite interpolation, post orthogonalisation and smoothing.
The yz-plane cross section of the near-field |E| distribution and the far-field scattering pattern ( Releft({mathbf{E}}^stimes {overline{mathbf{H}}}^scdot {mathbf{e}}_Rright){R}^2 ) as R → ∞ of the hybrid nanostructure consisting SI of (70, 70, 35) nm and SNP of r = 30 nm are shown in Fig. 3, where the incident angle is 45° and the excitation wavelength is 593 nm.
Left: cross section of the device with optical field distribution.
It depicts the cross section of the CTLE and WTLE O3VMR distribution along the 1st and the 180th meridian, respectively.
Open image in new window Fig. 7 X–Z cross section of the reservoir model showing saturation distribution in different layers.
A series of vertical cross-section of the distribution of S-wave velocity perturbation in the WNW-ESE direction (across the fault) is shown in Fig. 11.
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