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The repair/replacement cost of habitants, schools, hospitals, monuments, demolitions or temporary supports constitute 50.3%% of the total earthquake cost.
The 222Rn concentration was found to correlate well with the total earthquake energy within a 100-km radius of each fault.
The total earthquake loadingspreading over 31.18 s has been discretized into an interval of 0.02 s,thus resulting in 1,558 data points.
(a) Change of total earthquake energy with radius, determined using the earthquakes (Figure 1) within a radius from the center of measurement point locations.
(b) Positive correlation between the total earthquake energy and the median of the number of 222Rn for each active fault area.
This summation is termed the total earthquake energy (TEE .Among the earthquakes shown in Figure 1, those occurring within a circle of a given radius were selected to clarify the relationship between TEE and radius.
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In total 370 earthquake records belonging to 4 site conditions, with each containing 74 to 106 records, are used to calculate the structural response and finally the factor R. The structure periods vary from 0.1 to 6 s and the displacement ductility is taken to be 2, 3, 4, 5 and 6 respectively.
Then, if the combined model keeps the total expected earthquake rate (convex combination) unchanged, local rates cannot be higher (or lower) than the maximum (minimum) rates of the two models.
In total 972 earthquakes are recorded in the new catalogue, 200 from the years 1000 to 1899.
As a consequence of the cluster analysis, we obtained 278 clusters and 1,284 clustered earthquakes from a total of 4,523 earthquakes.
A low ratio of the number of small repeating earthquakes to the total number of earthquakes was observed in the area of large slip (Uchida et al., 2002), which is also suggestive of strong interplate coupling in this region.
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