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• W2002291261 abstract "Abstract Earthquake source theories of Haskell, Brune, and Savage have been drawn upon to develop a description of an earthquake as a major slip accompanied by many smaller tensional and slip events. We find natural explanations of several previously unexplained observations, such as: Robustness of the MS: mb discriminant, P corner frequency higher than S corner frequency for shallow earthquakes, High-frequency P/S amplitude ratio higher for shallow earthquakes than previous theories predict, Increase of complexity as a function of third moment, Small mb relative to MS for transform faults. (This can also be explained by emergent short-period P wave forms or by a low-Q region underlying the source). The theory predicts that MS:mb populations of earthquakes and explosions will not converge at small magnitudes. The theory also suggests that the standard interpretations of corner-frequency measurements can provide only a lower limit to fault-plane dimensions and, in combination with the moment, only an upper limit on stress drop." @default.
• W2002291261 created "2016-06-24" @default.
• W2002291261 creator A5031516916 @default.
• W2002291261 date "1975-10-01" @default.
• W2002291261 modified "2023-09-26" @default.
• W2002291261 title "A source theory for complex earthquakes" @default.
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• W2002291261 doi "https://doi.org/10.1785/bssa0650051385" @default.
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