Received wisdom relates that static stress change associated with an earthquake mainshock is the prime mover of its aftershocks. But a fresh look at the data points the finger at wave-surfing dynamic stress.
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References
Felzer, K. R. & Brodsky, E. E. Nature 441, 735–738 (2006).
Stein, R. S., King, G. C. P. & Lin, J. Science 265, 1432–1435 (1994).
Stein, R. R. Nature 402, 605–609 (1999).
Nalbant, S. S. et al. Nature 435, 756–757 (2005).
Dieterich, J. H. J. Geophys. Res. 84, 2161–2168 (1979).
Parsons, T. J. Geophys. Res 107, 2199; doi:10.1029/2001JB000646 (2002).
Huc, M. & Main, I. G. J. Geophys. Res. 108, 2324; doi:10.1029/2001JB001645 (2003).
Hubert-Ferrari, A. et al. Nature 404, 269–273 (2000).
Shearer, P., Hauksson, E. & Lin, G. Bull. Seismol. Soc. Am. 95, 904–915 (2005).
Parsons, T. A. Geophys. Res. Lett. 32, L04302 (2005).
Main, I. G. Geophys. J. Int. 142, 151–161 (2000).
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Main, I. A hand on the aftershock trigger. Nature 441, 704–705 (2006). https://doi.org/10.1038/441704a
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DOI: https://doi.org/10.1038/441704a