Open image in new window Fig. 12 Distribution of the maximum hydrodynamic pressures with different frequencies.
If a = n and b = 1, we obtain the distribution of the maximum.
Figure 5a shows the distribution of the maximum S-wave amplitudes of Event 1.
Figure 5c shows the spatial distribution of the maximum S-wave amplitude ratios for Events 2 and 3.
Figure 19 shows a plot of the vertical distribution of the maximum story-drift of the main frame.
Figure 4 shows the distribution of the maximum shear stress in the lower crust for our 6 cases.
According to the largest order statistics [15], the distribution of the maximum of the amplitude values is given by (4).
In addition, the location of the vertical crack also has a certain influence on the distribution of the maximum stress.
The distribution of the maximum shear strains in the shear zone showed good consistency with the fracture patterns of the tested samples.
They are relatively easy to implement and their form facilitates the development of a comprehensive and relatively straightforward theory for the asymptotic distribution of the maximum likelihood estimator.
We examined the spatial distribution of the maximum S-wave amplitudes during three earthquakes that occurred around the Bonin Islands (Events 1 3).
