Function G: alternative definition
The ratio of the number of earthquakes from
two magnitude ranges –
G(t½m1,m2,s) =
log( N(t | m2,s) / N(t | m1,s) ) / (m2 - m1)
l In such a definition G is the tangent of of
slope of frequency-magnitude graph.
Sixth Workshop on Non-Linear
Dynamics and Earthquake Prediction
The Abdus Salam ICTP, Miramare
16/10/2001
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