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Earthquakes nucleated by transient deformations caused by the M=7.9 Denali, Alaska, earthquake. Gomberg, J,Bodin, P,Larson, K,Dragert, H. Nature . 2004
[8]
Direct test of static stress versus dynamic stress triggering of aftershocks. Pollitz, F.F,Johnston, M.J.S. Geophysical Research Letters . 2006
[9]
A slow earthquake sequence on the San Andreas fault. Linde A T, Gladwin M T, Johnston M J S, et al. Nature . 1996