From the results of the Part I of this paper, the following study is made. First, the
b values of the four regions which express the characteristics of magnitude-frequency distribution are compared with each other. It is found that the
b values don't show any remarkable differences for each region and for each focal depth.
Second, the
m and β values which express the characteristics of amplitude-frequency distribution and seismic intensity-frequency distribution respectively, are obtained from the data of seismological stations near each region. These
m and β values are discussed in relation with the
b values.
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