The dynamics of the tectonic faults that produce earthquakes remain puzzling. An inference from laboratory experiments could help: at high rates of slip, friction at the interface may fall dramatically.
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Di Toro, G., Goldsby, D. L. & Tullis, T. E. Nature 427, 436–439 (2004).
Saffer, D. M., Bekins, B. A. & Hickman, S. J. Geophys. Res. 108, doi:10.1029/2002JB001849 (2003).
Scholz, C. H. Geology 28, 163–166 (2000).
Spray, J. G. J. Geophys. Res. 98, 8053–8068 (1993).
Mair, K. & Marone, C. J. Geophys. Res. 104, 28899–28914 (1999).
Lapusta, N. & Rice, J. R. Eos 84, S51B–02 (2003).
Heaton, T. Phys. Earth Planet. Inter. 64, 1–20 (1990).
Kanamori, H. & Heaton, T. H. in Geocomplexity and the Physics of Earthquakes (eds Rundle, J., Turcotte, D. L. & Kein, W.) AGU Monogr. 120, 147–155 (AGU, Washington DC, 2000).
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Marone, C. Faults greased at high speed. Nature 427, 405–406 (2004). https://doi.org/10.1038/427405a
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