They showed an increasing trend of Δ r c with the mainshock magnitude classes m ∈ [ M , M + 1), where M is magnitude, and Nanjo et al. used M = 3, 4, and 5, and compared it with the scaling relation between asperity size and M .
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Nucleation and Cascade Features of Earthquake Mainshock Statistically Explored from Foreshock Seismicity.
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