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Large earthquakes initiate by the acceleration of slips on the downward extensions of seismogenic faults

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Keywords: ductile deformation; earthquakes; foreshocks; lower crust; main shocks; slip rates

Document Type: Research Article

DOI: http://dx.doi.org/10.1016/S0012-821X(02)00709-4

Affiliations: Earthquake Research Institute, the University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, 113-0032, Tokyo, Japan

Publication date: September 15, 2002

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