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Statements
1983
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descriptive statistical model of earthquake source radiation
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estimation of short-period strong motion
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wide-band source spectrum scaling law
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various data sources
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lack of similitude
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two characteristic frequencies of about 0.2 and 5-10 Hz
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determine near-field accelerations
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formulae to estimate 'static' and wavefield accelerations of incoherently radiating sources
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average relation between maximum acceleration and intensity
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distance and magnitude
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