Seismic readings suggest that a zone of weak, slippery rocks lies beneath the Pacific northwest coast of the United States. These frail layers might be limiting the violence of earthquakes.
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Bostock, M. G., Hyndman, R. D., Rondenay, S. & Peacock, S. M. Nature 417, 536–538 (2002).
Peacock, S. M. & Hyndman, R. D. Geophys. Res. Lett. 26, 2517–2520 (1999).
Bose, K. & Ganguly, J. Earth Planet. Sci. Lett. 136, 109–121 (1995).
Giese, P., Scheuber, E., Schilling, F., Schmitz, M. & Wigger, P. J. S. Am. Earth Sci. 12, 201–220 (1999).
Yuan, X. et al. Nature 408, 958–961 (2000).
Bock, G., Schurr, B. & Asch, G. Geophys. Res. Lett. 27, 3929–3932 (2000).
Schmidt, M. W. & Poli, S. Earth Planet. Sci. Lett. 163, 361–379 (1998).
Ruff, L. J. & Tichelaar, B. W. in Subduction: Top to Bottom (eds Bebout, G., Scholl, D. W., Kirby, S. H. & Platt, J. P.) 105–111 (AGU, Washington DC, 1996).
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Zandt, G. The slippery slope. Nature 417, 497–498 (2002). https://doi.org/10.1038/417497a