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- W1992704312 abstract "We identify two distinct scaling regimes in the frequency–magnitude distribution of global earthquakes. Specifically, we measure the scaling exponent b = 1.0 for “small” earthquakes with 5.5 < m < 7.6 and b = 1.5 for “large” earthquakes with 7.6 < m < 9.0. This transition at mt = 7.6, can be explained by geometric constraints on the rupture. In conjunction with supporting literature, this corroborates theories in favor of fully self-similar and magnitude independent earthquake physics. We also show that the scaling behavior and abrupt transition between the scaling regimes imply that earthquake ruptures have compact shapes and smooth rupture-fronts." @default.
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- W1992704312 date "2012-04-01" @default.
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- W1992704312 title "A geometric frequency–magnitude scaling transition: Measuring b=1.5 for large earthquakes" @default.
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- W1992704312 doi "https://doi.org/10.1016/j.tecto.2012.01.034" @default.
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